302 Sentences With "cloudiness" | Random Sentence Generator

Global climate models tend to greatly underestimate the cloudiness of this region, and this makes the models relatively insensitive to possible changes in cloudiness.

The cloudiness of the water makes the heat even worse.

Transparent, perhaps, but it almost always has a bit of cloudiness to it.

Confidence: Medium On Friday, plan on partial cloudiness ahead of a gathering storm.

Cloudiness acts as an insulating blanket, preventing warmth from escaping the ground level.

If it were a colour, it'd be grey—the color of cloudiness and, usually, of reality.

Farrago becomes alarmed after seeing what he thinks is the cloudiness of blood in the urine sample.

An approaching cold front will bring considerable cloudiness Saturday morning, and rain is expected to begin then.

By contrast, places like India, southern Africa, or northern Australia experience massive swings in cloudiness throughout the year.

Cloudiness in the report led a Vermont electric utility to incorrectly believe an employee had been attacked by Russia.

In the midst of this cloudiness over my beliefs, I found my way to a church service on Easter Sunday.

During treatment, they both experienced what's sometimes called "chemo-fog," a general exhaustion and cloudiness that makes completing basic tasks difficult.

As of Sunday, the broad area of cloudiness, showers, and thunderstorms extended from western Cuba across the southeastern Gulf of Mexico.

Today (Friday): It's sunny in the morning, but we could see some afternoon cloudiness and snow showers as a Valentine's Day gift.

Like all dementia sufferers, he has moments of lucidity but when the cloudiness hits, I'm not sure he knows who he is.

We close out the week with some cloudiness and continued air stagnation, exacerbating some of our air-quality issues in the region.

Keep reading for the forecast into next week... Tomorrow (Saturday): Partly to mostly sunny skies may prove welcome news after our recent cloudiness.

Global climate models that predict 2 degrees of warming in response to doubling CO2 generally also see little or no change in cloudiness.

"Cloudiness or a change in taste or smell are signs of possible contamination," said Sue Dempsey, administrator of the department's Drinking Water Program.

A weather system approaches this weekend to deliver some cloudiness Saturday and then showers Sunday, but temperatures remain relatively warm, with highs in the 50s.

For tens of millions in the U.S. and abroad, the annual cosmic show will likely be partly to mostly blotted out by light pollution and cloudiness.

The weather bureau declares the arrival of monsoon rains only after measures including consistency of rainfall over a defined geography, intensity, cloudiness and wind speed are met.

But they're still short of the national production goals of 14.7 million bags, a shortfall the Colombian National Coffee Federation has attributed to excessive rain and cloudiness.

South Carolina has a greater-than-average chance of cloudiness, as does the region around the northern borders of Kansas and Missouri The agency also has a map that allows users to click for weather updates for any location along the path of totality, and an interactive map that shows the likelihood of cloudiness, based on historical data That interactive map is featured below, but is also available here.

The India Meteorological Department declares the arrival of monsoon rains only after parameters measuring consistency of rainfall over a defined geography, intensity, cloudiness and wind speed are satisfied.

So, if climate models were to take this new mechanism for forming aerosol particles into account, the contrast between present-day and pre-industrial cloudiness would be reduced.

In contrast to the violent motions of air within the areas of showers and thunderstorms surrounding the eye, the air within the eye sinks, scouring out any cloudiness.

The most common issue caused by the sun is cataracts, a cloudiness of the lens inside the eye, which can result in vision loss as we get older.

The India Meteorological Department (IMD) declares the arrival of monsoon rains only after parameters measuring consistency of rainfall over a defined geography, intensity, cloudiness and wind speed are satisfied.

The lack of sea ice and more ocean surface leads to additional cloudiness later in the fall season, which keeps the Arctic region warmer even later into the winter.

Although the long-range forecast is for increased cloudiness in the industry, tech companies should expect a light drizzle of investment, and not a downpour, until these worries are addressed.

Physicists therefore have to simplify or "parameterize" clouds in their global models, assigning an overall level of cloudiness to each grid cell based on other properties, like temperature and humidity.

The India Meteorological Department declares the arrival of monsoon rains only after parameters measuring the consistency of the rainfall over a defined geography, intensity, cloudiness and wind speed are satisfied.

Using the different physics of the two mechanisms, we showed that the combined effect of the two 'rival' hypotheses explained the changes in cloudiness more successfully than each would do individually.

But the introduction of softer blues and pinks, and of a cloudiness in the way those colors are applied, changes the tone, and these writhing figures could very well be dancing.

"We're still waiting for immediate measures, with a bigger and more effective scope, to fight the sediments that are in the rivers and reduce the intense cloudiness of the rivers," she said.

"Crybaby" has it all, while retaining a touch of the cloudiness that's always been a part of her work, all the way back to when she was recording goth-folk Gucci Mane covers.

This image shows how an 'iris clip', also known as an artificial intraocular lens (IOL), is used to treat conditions such as myopia (nearsightedness) and cataracts (cloudiness of the lens), is fitted onto the eye.

I love the long double filter that will keep all of the grounds in the filter (I even tried it with esspresso ground, it turned out to be fine with just a little cloudiness on the bottom).

The site also runs entirely on solar power (there's an image of the panel, which powers the site from Barcelona, below.) So if there's a long period of cloudiness in Barcelona, Low-Tech Magazine will go offline.

While natural wine is often unfiltered (that leads to cloudiness) and can veer sharply into funky territory, there's also lots of natural wine that won't feel like an acquired taste if you're used to buying yours at Costco.

Diaz folded at the midriff from the stinging body shots, and unable to launch any significant offense in such a vulnerable position, McGregor was able to take the round and shake some of the cloudiness from the third round.

Impurity-free ice grew in popularity after a core group of cocktail buffs like Dave Arnold, Don Lee, and Alex Day pioneered the concept—which emphasized creating a super-cold, slow-melting product that has no cracks, air bubbles, or cloudiness.

The researchers worked out a math model to represent all the pacemaker cells in our brain clock and accounted for inputs such as lights and how sensitive a person is to sunlight, cloudiness, geographical latitude and seasonal factors, therefore creating new circadian rhythms over various trajectories.

COLONIAL ERA MICHIGAN FORT REVEALS ITS SECRETS "We compared degradation that looked like corrosion versus a cloudiness from the residue from products used during the rinsing of the photographs during production versus degradation from the cover glass," Ian Coulthard, a co-author on the study, said in a statement.

Screens based on IGZO tech—which is an acronym for the indium gallium zinc oxide used to make Sharp's semiconductors—tend to have better transparency than silicon-based displays, which reduces the need for brighter backlighting, and could even help eliminate the cloudiness or haziness that often plagues the current Switch's screen.

"It's not enough to run a model of a little box and get some of the small scales correct; all of the intermediate factors have a strong influence on how the cloudiness evolves, and that's what's missing from that paper," says Bjorn Stevens, a director at the Max Planck Institute for Meteorology in Hamburg.

Olive oil cloudiness resulting from sediments discussed in this article is different from the characteristic cloudiness of olive oil due to storage at low temperatures [REF]. This type of cloudiness is the result of congealing of triglycerides. When these oils are returned to room temperature, they become again transparent. Unfiltered olive oil has a cloudy appearance that can persist months after the oil has been returned to room temperature.

Rough filtration leaves some cloudiness in the beer, but it is noticeably clearer than unfiltered beer. Fine filtration removes almost all cloudiness. Sterile filtration removes almost all microorganisms. ;Sheet (pad) filters These filters use sheets that allow only particles smaller than a given size to pass through.

If moisture is not sufficient, such as when a system has previously moved across a mountain barrier, cold fronts can pass without cloudiness.

Pirenoxine (abbreviated PRX, trade name Catalin) is a medication used in the possible treatment and prevention of cataracts. A report in the journal Inorganic Chemistry showed that in liquid solutions pirenoxine could cause decreased cloudiness of a crystallin solution produced to mimic the environment of the eye. Pirenoxine interacts with selenite or calcium ions that have been proven as factors leading to the formation of lens cataract. Pirenoxine reduces the cloudiness of the lens solution containing calcium by 38% and reduced the cloudiness of the selenite solution by 11%. “...there are not any proctored studies that prove the utility of these drops.

Patients with Reis-Bücklers dystrophy develop a reticular pattern of cloudiness in the cornea. This cloudiness, or opacity, usually appears in both eyes (bilaterally) in the upper cornea by 4 or 5 years of age. The opacity elevates the corneal epithelium, eventually leading to corneal erosions that prompt attacks of ocular hyperemia, pain, and photophobia. These recurrent painful corneal epithelial erosions often begin as early as 1 year of age.

Solar irradiance variability assessments are useful for solar power applications. Solar irradiance variability at any location over time is mainly a consequence of the deterministic variability of the sun's path across the sky dome and the variability in cloudiness. The variability of accessible solar irradiance on Earth's surface has been modeled using Markov chains, also including modeling the two states of clear and cloudiness as a two-state Markov chain.

In weaker tropical cyclones, the eye is less well-defined, and can be covered by high cloudiness caused by cirrus cloud outflow from the surrounding central dense overcast.

Malayan tapirs have very poor eyesight, making them rely greatly on their excellent sense of smell and hearing to go about in their everyday lives. They have small, beady eyes with brown irises on either side of their faces. Their eyes are often covered in a blue haze, which is corneal cloudiness thought to be caused by repetitive exposure to light. Corneal cloudiness is a condition in which the cornea starts to lose its transparency.

Furthermore, tree rings respond to multiple climatic effects (temperature, moisture, cloudiness), so that various aspects of climate (not just temperature) can be studied. However, this can be a double-edged sword.

Iquique has a rare desert climate (Köppen BWh) with low extremes of temperatures all year round and almost no rainfall. Being characterized by abundant cloudiness, it is sometimes classified as BWn, indicating a coastal desert climate with abundant cloudiness as the n denotes a climate with frequent fog. It is common for this place to almost have no rainy days in a year. It is one of the driest cities in the world, along with Arica.

The albedo of increased cloudiness cools the climate, resulting in a negative feedback; while the reflection of infrared radiation by clouds warms the climate, resulting in a positive feedback. Increasing temperatures in the polar regions is expected in increase the amount of low-level clouds, whose stratification prevents the convection of moisture to upper levels. This feedback would partially cancel the increased surface warming due to the cloudiness. This negative feedback has less effect than the positive feedback.

The presence of a large-scale high-pressure subtropical ridge on each side of the equator reduces cloudiness at these low latitudes. Similar patterns also occur at higher latitudes in both hemispheres.

During the rainy season, it remains heavily clouded. There is an increase of cloudiness from March onwards. A clear and cool weather starts appearing from September and remains till January the next year.

It generally stretches from the Solomon Islands through Vanuatu, Fiji, Samoa, and Tonga. Low-level convergence along this band forms cloudiness as well as showers and thunderstorms.Glossary of Meteorology. South Pacific convergence zone.

Cloud types are mainly low stratus and fog; cumuli forms are rare. Peak cloudiness occurs in August and September when the ocean is ice-free. Dense fog occurs an average of 65 days per year, mostly in the summer months.

The wave was notable in that it was almost completely devoid of any cloudiness or convection. The remnants of Cora crossed Central America and uneventfully continued westward until August 18, when its remains contributed to the formation of Hurricane Kristy.

The water first turns cloudy, but clears up once the infusoria eat the bacteria that caused the cloudiness. At this point, the infusoria are ready, and usually are visible to the naked eye as small, white specks swimming in the container.

The summer is warm and rainy. Autumn and spring are transitional seasons. Winter is the most cold season, with cloudiness around town and frequently polar air masses. Frosts occur sporadically in regions further away from the center, in some winters throughout the city.

Crystalluria refers to cloudy urine when the cause of cloudiness is due to crystals found in the urine when performing a urine test. Crystalluria is considered often as a benign condition and as one of the side effects of sulfonamides and penicillins.

Visitors often do not appreciate the sometimes-murky water in the lake, but the cloudiness represents a water column rich in microscopic life, providing a basis for a diverse and thriving web of animal life at the lake, both marine and avian.

Chill filtering is a method in whisky making for removing residue. In chill filtering, whisky is cooled to between , often roughly , and passed through a fine adsorption filter. This is done mostly for cosmetic reasons – to remove cloudiness – rather than to improve taste or consistency.

The second named storm of the season originated from a slow-moving area of increasing cloudiness over the Gulf of Tehuantepec on June 14. Moving little, a broad area of low pressure formed within the mass, but the low remained disorganized, although a tropical wave moved through on June 16. However, another tropical wave moved through on June 18, and the area of cloudiness gradually became more concentrated, and post-storm analysis indicated that a tropical depression formed on June 18 near Huatulco, as banding increased. A report of tropical storm-force winds from a ship was issued, and the depression was quickly upgraded to Tropical Storm Beatriz.

Parry Sound has a humid continental climate, with some quite- unusual local variations in cloudiness and precipitation for this climate, resulting from its location on the eastern shore of the large body of water comprising Parry Sound and Lake Huron to its west. Parry Sound's annual temperature regime reflects a cool-summer humid continental climate (Koppen Dfb), with January average temperatures of and July average temperatures near , and the usual minimal seasonal lag typical of continental climates, i.e. January as the coldest month, July as the warmest. Much more unusual (for Dfb climates) is Parry Sound's average annual cycle of precipitation, and cloudiness vs. sunshine.

The climate of the area can be locked in a mid-mountain Mediterranean climate. The average annual temperature is around 17 degrees. The rains are not abundant, around 400mm per year, but mountain ranges favor the formation of cloudiness and local rainfall, increasing these with altitude.

The climate of Cocos Island is mostly determined by the latitudinal movement of the Intertropical Convergence Zone, which creates cloudiness and precipitation that is constant throughout the year.Herrera, W. 1984. Informe de campo. Gira realizada a la Isla del Coco con el objetivo de recabar información climatológica.

Despite its cloudiness, and a relatively high frequency of rainy days, Invercargill receives less rain than either Auckland or Wellington. Invercargill is also New Zealand's second windiest city, after Wellington. The average temperature high ranges from in January to in July, but temperatures do occasionally exceed in summer.

Milankovitch, Milutin. Canon of Insolation and the Ice Age Problem. Zavod za Udz̆benike i Nastavna Sredstva: Belgrade, 1941. . The uneven solar heating (the formation of zones of temperature and moisture gradients, or frontogenesis) can also be due to the weather itself in the form of cloudiness and precipitation.

That would make the people dependent on the leader. If one wants to be saved, they should instead distance themselves from such organizations, self-reflect on aspects that are unharmonious to them in everyday life, and translate this into action. In doing so, by brushing away the cloudiness of one's soul one can receive the light of gods, and as an actual phenomenon, one is guided towards harmonization. “Tariki” (strength through others) constantly exists as compassion of God, but as it is not permitted for tariki to change one's consciousness, unless ones tries to receive the light of gods through their own will, this light will be closed off due to the “cloudiness” of their own soul.

Ames, IA. "Iowa Fact Sheet: Agriculture and Water Quality." October 2001. Document No. EDC232a. Sediment creates turbidity (cloudiness) in water bodies, reducing the amount of light reaching lower depths, which can inhibit growth of submerged aquatic plants and consequently affect species which are dependent on them, such as fish and shellfish.

A desert climate dominates the region. Near the coast, cloudiness can limit the temperature swing throughout the day, but in other drier areas, temperatures can vary greatly as is typical in deserts. A marginal desert region can be found over above sea level, which sees milder temperatures and summer rains.

Warm fronts are usually preceded by stratiform precipitation and fog. The weather usually clears quickly after a front's passage. Some fronts produce no precipitation and little cloudiness, although there is invariably a wind shift. Cold fronts and occluded fronts generally move from west to east, while warm fronts move poleward.

Visibility is merely or less on most summer afternoons because of the amount of water vapor in the air or because of cloudiness (fog). Days with afternoon visibility of or more are common only later in the fall and in winter.Jadwiga Orliczowa and Vladimír Peterka, "Dohľadnosť." In: Mikuláš Konček, et al.

He preached self- reflection as a means to do away with the cloudiness in one's soul (said to be created by humans' disharmonic ideas and actions) and to receive God's light, which the soul is said to originally receive. Takahashi then emphasized the practice of ideas and actions after self-reflection.

The high cloudiness between the dry season facilitates the formation of water vapor that compensates for the lack of rain. The trade winds that blow from the northeast provide rainfall over the highlands. Due to its proximity to the equator, the area's sunshine can be considered constant throughout the year.

A desert climate dominates the region. Near the coast, cloudiness can limit the temperature swing throughout the day, but in other drier areas, temperatures can vary greatly as is typical in deserts. A marginal desert region can be found over above sea level, which sees milder temperatures and summer rains.

This cloudiness, or opacity, causes the corneal epithelium to become elevated, which leads to corneal opacities. The corneal erosions may prompt attacks of redness and swelling in the eye (ocular hyperemia), eye pain, and photophobia. Significant vision loss may occur. Reis-Bücklers dystrophy is diagnosed by clinical history physical examination of the eye.

The trowal creates the portion of an occluded cyclone known as its comma head, due to the comma-like shape of the mid-tropospheric cloudiness that accompanies the feature. It can also be the focus of locally heavy precipitation, with thunderstorms possible if the atmosphere along the trowal is unstable enough for convection.

Light scattering and nephelometry are methods for the determination of the cloudiness of a solution (i.e.: insoluble particles in a solution). A light beam passes through the sample and the light is scattered by the suspended particles. The measured forward scattered light indicates the amount of the insoluble particles present in solution.

The climate of Azerbaijan is unique, as nine of the Earth's eleven climate zones are found in Azerbaijan.Climates of Azerbaijan Temperature, precipitation, humidity, evaporation and cloudiness all influence the landscape and climate of Azerbaijan. The climate varies considerably from east to west. In the western mountains, the weather is drier and more extreme.

The average annual rainfall ranges from very low in the northern and southern fringes of the desert to nearly non-existent over the central and the eastern part. The thin northern fringe of the desert receives more winter cloudiness and rainfall due to the arrival of low pressure systems over the Mediterranean Sea along the polar front, although very attenuated by the rain shadow effects of the mountains and the annual average rainfall ranges from to . For example, Biskra, Algeria, and Ouarzazate, Morocco, are found in this zone. The southern fringe of the desert along the border with the Sahel receives summer cloudiness and rainfall due to the arrival of the Intertropical Convergence Zone from the south and the annual average rainfall ranges from to .

A typical frontal passage is proceeded by increasing middle and high cloudiness with light rain. Following the frontal passage, mostly clear skies can be expected for 3 or 4 days. During this clear period it is very likely for fog to form. Fog is especially prevalent in river valleys and in low-lying areas.

Most of western Washington's weather is brought in by weather systems that form near the Aleutian Islands in Alaska. It contains cold moist air, which brings western Washington cold rain, cloudiness, and fog. November through January are Olympia's rainiest months. City streets, creeks, and rivers can flood during the months of November through February.

Kieselguhr, a fine powder of diatomaceous earth, can be introduced into the beer and circulated through screens to form a filtration bed. Filtration ratings are divided into rough, fine, and sterile. Rough filters remove yeasts and other solids, leaving some cloudiness, while finer filters can remove body and color. Sterile filters remove almost all microorganisms.

Experimentally, the phase separation can be followed by turbidimetry. There is no universal approach for determining the cloud point suitable for all systems. It is often defined as the temperature at the onset of cloudiness, the temperature at the inflection point of the transmittance curve, or the temperature at a defined transmittance (e.g., 50%).

MEI is determined as the first principal component of six different parameters: sea level pressure, zonal and meridional components of the surface wind, sea surface temperature, surface air temperature and cloudiness using data from the International Comprehensive Ocean-Atmosphere Data Set (ICOADS ).Wolter, Klaus. "Multivariate ENSO Index (MEI)." NOAA Earth System Research Laboratory - Physical Sciences Division.

A 2015 study found that artificial cloudiness caused by contrail "outbreaks" reduce the difference between daytime and nighttime temperatures. The former are decreased and the latter are increased, in comparison to temperatures the day before and the day after such outbreaks.Bernhardt, J. & Carleton, A.M. (2015). The impacts of long-lived jet contrail ‘outbreaks’ on surface station diurnal temperature range.

Near bottom plumes occur when the tailings are pumped back down to the mining site. The floating particles increase the turbidity, or cloudiness, of the water, clogging filter-feeding apparatuses used by benthic organisms. Surface plumes cause a more serious problem. Depending on the size of the particles and water currents the plumes could spread over vast areas.

Winters are mild with frequent frosts and cold spells. Temperatures are usually mild during the day and cold during the night. Most precipitation results from frontal systems associated with cyclogenesis and sudestada, which bring long periods of precipitation, cloudiness and cooler temperatures, particularly in the southern and eastern parts. Dull, gray and damp weather characterize winters in the Pampas.

In mid-September, a weak tropical wave moved off the coast of Northwest Africa. It moved westward and entered the eastern Pacific Ocean early on September 23. Cloudiness became concentrated with the system south of the Gulf of Tehuantepec. On September 27, the organized thunderstorm area was upgraded to Tropical Depression Twenty One-E while south of Acapulco.

A tropical wave moved off the northwest coast of Africa on June 5. It continued westward across the tropical North Atlantic and Caribbean Sea without significant development. The wave entered the northeastern Pacific Ocean on June 16, where it generated an area of increased cloudiness. Organization of thunderstorm activity increased late on June 18 and early on June 19.

Near-bottom plumes occur when the tailings are pumped back down to the mining site. The floating particles increase the turbidity, or cloudiness, of the water, clogging filter-feeding apparatuses used by benthic organisms. Surface plumes cause a more serious problem. Depending on the size of the particles and water currents the plumes could spread over vast areas.

Similarly, winter flights account for only 22% of annual air traffic, but contribute half of the annual mean radiative forcing. A 2015 study found that artificial cloudiness caused by contrail "outbreaks" reduces the difference between daytime and nighttime temperatures. The former are decreased and the latter are increased, in comparison to temperatures the day before and the day after such outbreaks.

Frequencies of departure appear to be affected by environmental factors such as cloudiness or rain. In addition, the foraging activities of A. flavissima correspond with phases of the moon as frequency of foraging significantly increases during the full and last quarter moon. This indicates that the presence of light is an important determinant of the nocturnal activities of the species.

The lowest mean monthly temperature in Zenica was in January 1964 [; minimal in January 1963] and maximal mean monthly temperatures were registered in August 2003 [; maximal in August 2003]. Relative air humidity is 70% and cloudiness 6.1 tenths. Air pressure is 976.3 millibars. Zenica has one meteorological station; it was founded in 1925 and is located at an elevation of a.s.l.

Tropical Depression Winnie was a weak, but catastrophic tropical cyclone that killed nearly 1,600 people after triggering widespread flooding in the Philippines. It was the second deadliest tropical cyclone of 2004 worldwide, only surpassed by Atlantic Hurricane Jeanne. A depression, which formed east of Samar, brought heavy rain to areas where it passed through, and affecting many areas, owing to Winnie’s large cloudiness.

Tropical cyclones with maximum sustained winds between and can have their center of circulations obscured by cloudiness within visible and infrared satellite imagery, which makes diagnosis of their intensity a challenge. Winds within tropical cyclones can also be estimated by tracking features within the CDO using rapid scan geostationary satellite imagery, whose pictures are taken minutes apart rather than every half-hour.

Sadler was the author of many books and essays on tropical meteorology including Average Cloudiness in the Tropics from Satellite Observations (1969) and Pacific Ocean Cloudiness from Satellite Observations (1976). Sadler documented the tropical cyclones over the eastern North Pacific that were revealed by satellite observations, and suggested that the upper-tropospheric circulation is a factor of development, as well as the life history of the tropical cyclones. Using charts of mean 200-hectopascal circulation for July through August to locate the circumpolar troughs and ridges, he observed that there is a trough line extending over the eastern and central North Pacific and another one extending over the North Atlantic. He also stated that the summer tropical upper tropospheric trough in the Southern Hemisphere lies over the trade wind region of the east central Pacific and can induce tropical cyclones.

According to press reports from Mexico City, the hurricane was considered the worst system to affect the state since the dawn of the 20th century. Moisture from this hurricane passed into the southwestern United States, where it caused rain of up to in the mountains and deserts of California. From September 16 to 22, cloudiness and showers were reported along the southern portion of the state.

Secondary lens luxation is caused by trauma to the eye and is not hereditary. The condition appears in a number of terrier breeds as well as the Border collie, Brittany and Cardigan Welsh corgi. Cataracts can affect any breed of dog and is the same condition as seen in humans. Here the lens of the eye hardens and is characterised by cloudiness in the eye.

Although the spider can have white-colored stripes, it does not possess the same UV properties as the closely related Gasteracanthra cancriformis. Different colored morphs inhabit different regions of the rainforest habitat with varying frequencies. Changes in light exposure of brighter forest clearings and cloudier sky overhang regions, create microhabitats for the Gasteracantha fornicata. Levels of cloudiness serve as a threshold marker for color morph frequency.

Air pressure In worldwide weather charts there are shown weather data like wind speed, air pressure (isobars), etc., each actualised two to three times per day, and with weather forecast up to three days. For each harbor there is a Meteogram with detailed wind forecasts and weather information for eight days. Available weather data for wind direction, wind speed, air temperature, air pressure, relative humidity, cloudiness, precipitation.

Arctic Fronts form in the Arctic region, and move southwards in southerly flows. When they reach Northern Europe, they have usually travelled over an open sea, and convective cloudiness has developed. The appearance of an Arctic Cold Fronts is then, essentially, that of a shallow Cold Front. Arctic Cold Fronts are usually so far north that Meteosat images alone are inadequate to recognize them.

Some fronts produce no precipitation and little cloudiness, although there is invariably a wind shift. Cold fronts and occluded fronts generally move from west to east, while warm fronts move poleward. Because of the greater density of air in their wake, cold fronts and cold occlusions move faster than warm fronts and warm occlusions. Mountains and warm bodies of water can slow the movement of fronts.

Filamentous opacities appear in the cornea with intertwining delicate branching processes. During an eye examination, the doctor sees these deposits in the stroma as clear, comma- shaped overlapping dots and branching filaments, creating a lattice effect. Over time, the lattice lines will grow opaque and involve more of the stroma. They will also gradually converge, giving the cornea a cloudiness that may also reduce vision.

Later that day, Hallie merged with a frontal zone and became extratropical offshore Virginia. The precursor to Hallie produced extensive cloudiness precipitation in the Bahamas. On October 27, gale warnings were issued for portions of the Outer Banks of North Carolina, and small craft advisories were posted for coastal areas from Georgia to Virginia. Tides along the North Carolina and Virginia coasts were generally between above normal.

On November 1, an area of disturbed weather – a mass of cloudiness and thunderstorms – developed over the western Caribbean Sea. Subsequently, a low pressure area began to form. The system was designated a tropical depression early on November 3, while located about to the south of the Cayman Islands. Operationally, the National Hurricane Center began issuing advisories on the tropical depression at on November 3\.

Hurricane Rick's ultimate origin was a tropical wave that left Africa on October 15. While crossing the Atlantic, the wave was mainly tracked by continuity due to its lack or organization. After entering the Pacific, part of it developed cloudiness on November 5 when it was south of the Gulf of Tehuantepec. Organization and a circulation developed, and satellite tracking began on November 6.

Mean winter precipitation ranges from less than in the west to over in the eastern parts. Unlike summer and spring where precipitation mainly falls from convective thunderstorms, most of the precipitation during winter comes from frontal systems, particularly the Sudestada which often bring long periods of precipitation, cloudiness, cooler temperatures and strong winds. Spring (September–November) is similar to fall, with a mean precipitation of .

Some fronts produce no precipitation and little cloudiness, although there is invariably a wind shift. Cold fronts and occluded fronts generally move from west to east, while warm fronts move poleward. Because of the greater density of air in their wake, cold fronts and cold occlusions move faster than warm fronts and warm occlusions. Mountains and warm bodies of water can slow the movement of fronts.

The area experiences lake effect weather, primarily in the form of increased cloudiness during late fall and early winter. The monthly daily average temperature in July is , while the same figure for January is . Temperatures reach or exceed on 10 days, and drop to or below on 4.6 nights. Precipitation tends to be the heaviest during the summer months, but most frequent during winter.

Brushfield spots, visible in the irises of a baby with Down syndrome Hearing and vision disorders occur in more than half of people with Down syndrome. Vision problems occur in 38 to 80%. Between 20 and 50% have strabismus, in which the two eyes do not move together. Cataracts (cloudiness of the lens of the eye) occur in 15%, and may be present at birth.

With professor Robert Herman, he also developed the basis of the two fluid model, a traffic model in traffic engineering for urban networks, analogous to the two fluid model in classical statistical mechanics. Prigogine's formal concept of self-organization was used also as a "complementary bridge" between General Systems Theory and thermodynamics, conciliating the cloudiness of some important systems theory concepts with scientific rigour.

It is located in the tropics but its high altitude modifies this to a warm temperate climate. The average annual temperature is .Average monthly data 1971 - 2000, GHCN Climate averages As with much of the Highveld, summers are long but not hot as the temperature depends on the amount of cloudiness and indirectly the amount of rain received. Drought years are hotter than wet years.

Sea spray heavily damaged fruit trees and rice paddies. Crop damage amounted to $3 billion, mostly to the apple industry, after 345,000 tons of apples fell to the ground and another 43,000 were damaged on the trees. Most farms lost 80% of their crop, potentially taking 10 years to regrow. Persistent cloudiness and rainfall following the storm diminished sunlight by 50%, furthering crop damage.

Deep puddles, thick mud, and landslides along roads form barriers to transportation. Cold winds, low temperatures at night, and moderate temperatures during the day, cloudiness, light showers and snowfall mark winter weather in this zone. Fog causes poor visibility, which poses a threat to vehicular traffic in the city. As spring approaches, the landscape is marked by violent winds and relatively dry and clear skies.

A tropical wave came off the northwest coast of Africa on May 20. The wave did not significantly develop as it moved west across the Atlantic Ocean and Caribbean Sea. Once it crossed Central America into the eastern Pacific Ocean, cloudiness increased considerably with the system on May 31. It became well- enough organized to be upgraded to Tropical Depression Two-E on June 2.

A tropical wave came off the coast of Africa into the eastern Atlantic Ocean on June 10 and 11. The system moved across the Atlantic and entered into the northeastern Pacific Ocean. The wave became a significant tropical system, with cyclonic turning in the lower and middle layers of the system's cloudiness on June 25. The center of circulation was located south of Acapulco, Mexico.

Raduga (in Russian Радуга, Rainbow) is the codename of a Soviet thermonuclear test, conducted on October 20, 1961, in Mityushikha Bay, Severny Island of Novaya Zemlya. The test was conducted by the Northern Fleet. An R-13 missile with a thermonuclear warhead was fired from the submarine K-102. When the submarine reached the specified point in the Barents Sea, she could not establish her position due to cloudiness and snowfall.

Following the swamp's collapse, its geomorphology changed dramatically, the peat fractured and a major channel was formed on its northern side. The vegetation was highly disturbed and bare peat was exposed. Turbidity (cloudiness) in the adjoining reservoir was over 300 NTU. A few months later willows (Salix sp.) growing on the margin of the swamp seeded and there was an explosion of willow seedlings germinating in the nutrient-rich bare peat.

Modern climate change is driven by the human emissions of greenhouse gas from the burning of fossil fuel driving up global mean surface temperatures. Rising temperatures are only one aspect of modern climate change though, with includes observed changes in precipitation, storm tracks and cloudiness. Warmer temperatures are driving further changes in the climate system, such as the widespread melt of glaciers, sea level rise and shifts in flora and fauna.

The average annual precipitation is . On average, precipitation falls on 60 days each year in Fair Oaks, and nearly all of this falls during the winter months. Average January rainfall is , and measurable precipitation is rare during the summer months. On rare occasions, monsoonal moisture surges from the Desert Southwest can bring upper-level moisture to the Sacramento region, leading to increased summer cloudiness, humidity, and even light showers and thunderstorms.

During an eye examination, the doctor sees these deposits in the stroma as clear, comma-shaped overlapping dots and branching filaments, creating a lattice effect. Over time, the lattice lines will grow opaque and involve more of the stroma. They will also gradually converge, giving the cornea a cloudiness that may also reduce vision. In some people, these abnormal protein fibers can accumulate under the cornea's outer layer—the epithelium.

On September 25, 1998 a tropical wave emerged off the coast of Africa, producing intermittent concentrated clusters of convective activity. The wave traversed the Atlantic Ocean and the Caribbean Sea before crossing Central America on October 5 or October 6. After several days, convection increased, and Dvorak classifications initiated. Satellite imagery indicated that the system dissipated on October 11, although an area of cloudiness persisted off the coast of Mexico.

Before Iana formed, there was a persistent area of cloudiness across the Mozambique Channel in late February. A low pressure area originated over eastern Mozambique and moved eastward over water, emerging near Beira. On February 25, a tropical disturbance formed off the west coast of southern Madagascar and moved east-northeastward, steered by a ridge to the south. Shortly thereafter, the center passed just north of Europa Island.

Washed out road in Saint-Pierre, Réunion For twelve days, the circulation of the storm produced cloudiness and thunderstorms over Réunion. Hyacinthe broke several rainfall records for tropical cyclones, becoming the wettest tropical cyclone on record. From January 14 to January 28, the storm dropped at Commerson Crater, just north of the Piton de la Fournaise volcano. Over ten days, Hyacinthe produced 5,678 mm (223.5 in), also at Commerson.

Fibrillogenesis can be analyzed through the use of turbidity tests. Turbidity is way of measuring the haziness, cloudiness, or fogginess of sample and also can be used to test the light-scattering properties of said sample. A turbidity test on fibrillogenesis will start with a sample of collagen triple-helices, which will have a low-level of turbidity. After fibrillogenesis is completed, the triple-helices will have formed fibrils.

On April 28, a stationary front drifted across the central United States, associated with cloudiness and showers. By 21:00 UTC, a surface low with a central pressure of developed in central Kansas. Shortly afterwards, thunderstorms erupted along the stationary front, which required the National Weather Service to issue some severe weather watches. A few tornadoes touched down, including an EF2 that caused considerable damage near Cameron, Oklahoma.

Autumn is one of the rainiest seasons, with many places receiving over . As in summer, precipitation falls mainly during convective thunderstorms. Winter is the driest season, with precipitation ranging from less than in the west to over in the east. Most of the precipitation during winter comes from frontal systems, particularly the sudestada (Spanish for strong southeasterly winds), bringing long periods of rain, cloudiness, cooler temperatures, and strong winds.

A convective area of cloudiness existed northeast of the Bahamas in mid July in response to a stationary frontal boundary. On July 15, satellite imagery suggested the presence of a weak circulation within the system. Around 00:00 UTC on the following day, a subtropical depression formed about northeast of the Bahamas. Moving northeastward, the cyclone slowly strengthened, becoming a subtropical storm at about 12:00 UTC on July 17\.

Hurricane Lily was a short-lived Category 1 hurricane of August 1971 that devastated the city of Puerto Vallarta in Mexico. Forming from an area of cloudiness associated with former Atlantic Tropical Storm Chloe, the storm slowly intensified, building to peak intensity just before landfall northwest of Manzanillo, Colima on August 31. The hurricane quickly weakened and became extratropical. After leaving land, the extratropical remnants of Lily dissipated on September 1.

Kevin formed from a westward-moving tropical wave which emerged from the northwest coast of Africa on September 11. The wave crossed into the Pacific basin on September 21 with no signs of development. Cloudiness and convection became better organized on the first hours of September 24, becoming Tropical Depression Thirteen-E the next day as it was located about southeast of Acapulco. Then the depression moved toward the west.

The number of clear nights (zero cloudiness) at the Wise Observatory site is about 170 a year. The number of useful nights, with part of the night cloud-free, is about 240. The best season, when practically no clouds are observed, is June to August, while the highest chance for clouds are in the period January to April. Winds are usually moderate mainly from North-East and North.

Upon moving ashore near Quintana Roo, the system spread cloudiness and precipitation across much of the Yucatán Peninsula, resulting in widespread flooding. In southern Mexico, Chiapas received rainfall amounts of 9.3 in (237 mm) in Tapachula and Soconusco over a 36-hour time span. Floods, landslides, and strong winds damaged more than 450 homes in the state. Emergency workers evacuated about 150 families after two rivers in the region reached dangerous water levels.

Patients diagnosed with Meesmann corneal dystrophy are unable to tolerate the use of contact lenses which irritate the corneal epithelium. Light microscopy and electron microscopy found that the basement membrane is thickened with an intracytoplasmic substance. Under slit-lamp photography, the cornea was found to be uneven due to the damage and scarring from the thickening basement membrane and anterior stroma. The buildup of foreign materials may cause vision blurriness or cloudiness.

La Serena has a cool desert climate, similar to nearby places in that it is clearly seasonal – in summer there is an absence of precipitation, but with abundant morning cloudiness and drizzle. which dissipates around noon, giving way to clear skies and days. In winter, the temperatures descend to between . Being located in a coastal zone, the minimums and maximums are moderated by the maritime influence and the temperature of the cold Humboldt Current.

Late on September 13, an area of convectional cloudiness persisted near the same position where Kalmaegi formed. The next day, JTWC upgraded it as a tropical disturbance. The system entered an area of moderate vertical windshear and towards warm waters, as it was upgraded to a tropical depression by the JMA early on September 17. On the same day, the depression moved into the Philippine Area of Responsibility and was locally named Mario.

As a consequence of humans emitting greenhouse gases, global surface temperatures have started rising. Global warming is an aspect of modern climate change, a term that also includes the observed changes in precipitation, storm tracks and cloudiness. As a consequence, glaciers worldwide have been found to be shrinking significantly. Land ice sheets in both Antarctica and Greenland have been losing mass since 2002 and have seen an acceleration of ice mass loss since 2009.

Most of the moisture is dropped on the Chilean side, causing abundant precipitation and cloudiness while on the Argentine side, the air warms adiabatically, causing it to become drier as it descends. Thus, an extensive rain–shadow is present in much of Patagonia, causing it to receive very little precipitation. The Sierras Pampeanas influences the climate on a much smaller scale than the Andes. Distance from the sea is another important geographic factor.

Thereafter the humidity decreases and in the summer the air is very dry. Cloudiness: During the monsoon season, and for brief spells of a day or two in association with passing disturbances in winter, heavily clouded or overcast skies prevail. In the rest of the year, the skies are mostly clear or lightly clouded. Winds: Winds are in general very light with a slight increase in force in the late summer and monsoon seasons.

The town is situated on Zimbabwe's Highveld at an altitude of , above sea level. It is located in the tropics but its high altitude modifies this to a warm temperate climate. The average annual temperature is .Average monthly data 1971 – 2000, GHCN Climate averages As with much of the Highveld, summers are long but not hot as the temperature depends on the amount of cloudiness and indirectly the amount of rain received.

Sunsets in Azerbaijan are often very colorful. The Azerbaijani plains and foothills have high insolation rates. The sun shines for 2,200 to 2,400 hours annually on the Kur- Araz lowland, Apsheron peninsula and other plains and foothills, and 2,600 to 2,800 hours on the plains around the Araz river in the Nakhchivan region. Due to increased cloudiness in the mountainous regions, those areas receive only 1,900 to 2,200 hours of direct sunlight.

In February 1992, Sacramento had 16 consecutive days of rain, resulting in an accumulation of for the period. On rare occasions, monsoonal moisture surges from the Desert Southwest can bring upper-level moisture to the Sacramento region, leading to increased summer cloudiness, humidity, and even light showers and thunderstorms. Monsoon clouds do occur, usually during late July through early September. Sacramento is the second most flood susceptible city in the United States after New Orleans.

A ridge behind the trough steered the weakening system to the northwest, causing Chantelle to reach the low latitude of 5° S. Widespread cloudiness made it difficult for MFR to continue tracking the circulation, and the agency issued the final advisory on November 30 northwest of Diego Garcia. The JTWC continued tracking the storm for several more days, and the remnants of Chantelle likely contributed to the formation of the subsequent Tropical Cyclone Daniella.

Racking is done for two reasons: it lets the mead sit away from the remains of the yeast cells (lees) that have died during the fermentation process. Second, this lets the mead have time to clear. The cloudiness could have been caused by either yeast or suspended protein molecules. There also the possibility that the pectin from any fruit that is used could have set which gives the mead a cloudy look.

Due to the high altitude, temperatures in Hazara are cooler than on the plains, though Abbottabad at still has maxima around 32 °C (90 °F) with high humidity in June and July. Further up, temperatures are cooler, often cooler than the Northern Areas valleys due to the cloudiness. In winter, temperatures are cold, with minima in January around 0 °C (32 °F) and much lower in the high mountains. Snowfalls are not uncommon even at lower levels.

A tropical wave that led to the formation Atlantic Hurricane Felix over the eastern Atlantic on September 7 also seems to have produced Kiko. This wave moved westward at low latitudes, crossing northern South America on September 13 – September 14 and Central America on September 15 and September 16. By September 17, cloudiness and showers increased near the Gulf of Tehuantepec. The area of disturbed weather moved westward for the next few days, without much increase in organization.

Her tongue has been crudely cut out, one of her molars is missing, her lungs are blackened as though she had suffered third degree burns, and her internal organs reveal numerous cuts and scarring. Jimsonweed, a paralyzing agent not native to the area, is found in her stomach. The condition of much of the body suggests that death had just occurred, while cloudiness of the corpse's eyes suggests she has been dead for several days. Other mysterious events occur.

The normal filtration ratings are defined as rough, fine or sterile. Rough filtration leaves some cloudiness in the beer, but it is noticeably clearer than unfiltered beer. Fine filtration yields a beer which is nearly transparent and not cloudy, although observation of the scattering of light through the beer will reveal the presence of some small particles. Finally, as its name implies, sterile filtration is fine enough that almost all microorganisms in the beer have been removed.

The cornea is necessary for the transmitting and focusing of outside light as it enters the eye, and cloudiness can cause vision loss. This causes the Malayan tapir to have very inadequate vision, both on land and in water, where they spend the majority of their time. Also, as these tapirs are most active at night and since they have poor eyesight, it is harder for them to search for food and avoid predators in the dark.

Divergence is the opposite of convergence. In the Earth's troposphere, it involves the horizontal outflow of air from the upper part of a rising column of air, or from the lower part of a subsiding column often associated with an area or ridge of high pressure. Cloudiness tends to be least prevalent near the poles and in the subtropics close to the 30th parallels, north and south. The latter are sometimes referred to as the horse latitudes.

Early on September 25, an area of convectional cloudiness associated with the monsoon through formed to the southeast of Palau. Satellite imagery showed a consolidating Low Level Circulation Centre. On September 27, the system began improving and showing a partial LLCC due to favorable conditions and was also located under moderate vertical wind shear, whilst the JMA upgraded the system into a tropical depression. On the evening of that day, the JTWC issued a Tropical Cyclone Formation Alert.

On September 28, an area of convectional cloudiness formed to the northeast of Pohnpei. Satellite imagery showed a Low Level Circulation Centre had begun to form. On the evening of September 28, due to a TUTT that was providing good outflow for the system and low-level vertical wind shear with a favorable environment, the JTWC issued a Tropical Cyclone Formation Alert. Early on September 29, both JMA and JTWC upgraded the system into a tropical depression.

130px Maxillary sinusitis is inflammation of the maxillary sinuses. The symptoms of sinusitis are headache, usually near the involved sinus, and foul-smelling nasal or pharyngeal discharge, possibly with some systemic signs of infection such as fever and weakness. The skin over the involved sinus can be tender, hot, and even reddened due to the inflammatory process in the area. On radiographs, there is opacification (or cloudiness) of the usually translucent sinus due to retained mucus.

A tropical wave moved off the northwestern coast of Africa into the Atlantic Ocean on August 11. After moving across the Atlantic and Caribbean Sea without development, the system moved through the Intertropical Convergence Zone of the northeastern Pacific Ocean. The cloudiness moved northward toward the Gulf of Tehuantepec on August 22. The thunderstorm activity organized sufficiently for the system to be upgraded to Tropical Depression Fifteen-E on August 23 while southeast of Acapulco, Mexico.

By mid-afternoon, inland areas have heated sufficiently to decrease the air pressure and increase the onshore flow. By late afternoon, the wind increases and begins to cool the onshore marine layer, allowing the fog and low clouds offshore to progress inland without evaporating. Cloudiness streams in over the Bay and through the various gaps. How far the clouds can penetrate inland depends on the depth of the marine layer and the strength of the cooling winds.

The recent practice of Independent Catholic groups to ordain women has added a definite cloudiness to the recognition of the validity of orders, as the act of ordaining women as priests or bishops is incompatible with Catholicism and Eastern Orthodoxy. The practice by some independent clergy of receiving multiple ordinations also demonstrates an understanding of Holy Orders which is at variance with Catholicism and Orthodoxy, both of which hold that a person is either ordained or not.

MOS can correct for local effects that cannot be resolved by the model due to insufficient grid resolution, as well as model biases. Because MOS is run after its respective global or regional model, its production is known as post-processing. Forecast parameters within MOS include maximum and minimum temperatures, percentage chance of rain within a several hour period, precipitation amount expected, chance that the precipitation will be frozen in nature, chance for thunderstorms, cloudiness, and surface winds.

A tropical wave developed over western Africa near the Prime meridian on September 14\. Two days later, residual cloudiness and sounding data from Dakar, Senegal, indicated that the system entered the Atlantic Ocean. After the system quickly developed deep convection and improved significantly in organization, it was classified as Tropical Depression Nine starting at 0000 UTC on September 19, while located approximately southwest of Cape Verde. The depression initially tracked west to west-southwestward with slow intensification, due to vertical wind shear.

Reis-Bücklers corneal dystrophy, is a rare, corneal dystrophy of unknown cause, in which the Bowman's layer of the cornea undergoes disintegration. The disorder is inherited in an autosomal dominant fashion, and is associated with mutations in the gene TGFB1. Reis-Bücklers dystrophy causes a cloudiness in the corneas of both eyes, which may occur as early as 1 year of age, but usually develops by 4 to 5 years of age. It is usually evident within the first decade of life.

Maceration of herbs and fruits was now moved to chrome steel tanks. The time of maceration for a typical batch ranges from 1 to 5 years. After filtration the liquor is further matured for 2–3 years. As all ingredients of the Sơn Tinh liquors are natural, and cold-filtration is avoided to preserve the full flavour, some sedimentation might appear in the bottled products, or the liquor might show some cloudiness when cooled to very low temperatures or when water is added.

Cold stabilization causes tartrates to crystallize and precipitate out of the wine. As a complex chemical mixture dependent on the activity of microorganisms, wine can be unstable and reactive to changes in its environment. Once bottled, a wine may be exposed to extremes of temperature and humidity, as well as violent movement during transportation and storage. These may cause cloudiness, sedimentation and/or the formation of tartrate crystals; more seriously, they may also cause spoilage or the production of carbonic gas.

Yazd has a hot desert climate (Köppen climate classification BWh). It is the driest major city in Iran, with a yearly precipitation amount of and only 23 days of precipitation, with summer temperatures very frequently above in blazing sunshine with no humidity. Even at night the temperatures in summer are rather uncomfortable. In the winter, the days remain mild and sunny, but in the morning the thin air and low cloudiness cause cold temperatures that can sometimes fall well below .

Cirrus clouds have been observed to develop after the persistent formation of contrails and have been found to have a global warming effect over-and-above that of contrail formation alone. The contribution of contrail and cirrus cloud formation to global warming is uncertain, and attempts to estimate aviation's overall climate change contribution do not tend to include its effects on cirrus cloud enhancement. A 2015 study found that artificial cloudiness caused by contrail "outbreaks" reduces the difference between daytime and nighttime temperatures.

The timing of the transition also influences changes in sea ice, ozone, air temperature, and cloudiness. Early and late polar breakup episodes have occurred, due to variations in the stratospheric flow structure and upward spreading of planetary waves from the troposphere. As a result of increased waves into the vortex, the vortex experiences more rapid warming than normal, resulting in an earlier breakup and spring. When the breakup comes early, it is characterized by with persistent of remnants of the vortex.

It has a relatively homogeneous climate, where the average minimum temperature varies between 20º and 35ºC., being this one regulated by the winds coming from the gulf of Venezuela and the trade winds that go up the Llanos, which produce areas of cloudiness and frequent torrential rains. A typical Sabana climate of the plain area of Venezuela where Guanare is located. It has two well-defined periods, a dry period from December to April, and a rainy period from May to November.

On August 19, the JMA briefly monitored a tropical depression, that had developed along the coast of China to the northeast of Hong Kong. During August 24, from a post-analysis by the JMA, a tropical depression had developed well to the southeast of Tokyo, Japan. The system dissipated on August 26 as it was absorbed by a cold front associated with an extratropical system to its north. Convectional cloudiness persisted over the Philippines, contributing to bring heavy rainfall on August 25.

At the same time, JTWC downgraded Parma into a tropical storm while the JMA downgraded it into a severe tropical storm. Early the next day, satellite imagery revealed that Parma had an eye center but no convectional cloudiness due to high pressure. Intensification was unlikely because of unfavorable environment conditions and interaction with Typhoon Melor. On October 6, at 11:00 pm PST (15:00 UTC), Parma made its second landfall over Ilocos Norte as it moved to the southeast.

Snowfall can occur, primarily from December to March, but snow accumulation is rarely heavy and usually short-lived. The exposed North Atlantic location and proximity to autumn and winter storm tracks means high winds are a regular occurrence, alongside high levels of cloudiness and precipitation. The weather station is at an elevation of , so temperatures are likely to be slightly milder in the town centre at sea level. Owing to its northerly location, winter months are extremely dark in Lerwick.

On August 10, Tropical Storm Bret made landfall in Nicaragua with maximum sustained winds of . Moving quickly inland, Bret weakened to a tropical depression, and dissipated over the mountainous terrain of Central America. Moving off towards west, convection associated with the remnant area of cloudiness developed in intermittent bursts, but by August 14, a more steady trend of development was observed. While centered south-southeast of Manzanillo, it is estimated that a tropical depression formed around 0000 UTC August 15.

Model output statistics differ from the perfect prog technique, which assumes that the output of numerical weather prediction guidance is perfect. MOS can correct for local effects that cannot be resolved by the model due to insufficient grid resolution, as well as model biases. Forecast parameters within MOS include maximum and minimum temperatures, percentage chance of rain within a several hour period, precipitation amount expected, chance that the precipitation will be frozen in nature, chance for thunderstorms, cloudiness, and surface winds.

Further cooling is caused by the high amount of cloudiness. The sea starts to freeze in late September and reaches its annual maximum in March, at which time ninety-five percent of the sea is ice-covered. The ice starts to decrease in May and suffers a major melting in June, with the minimum occurring in August or early September.Barr (1995): 11 During winter, high-pressure weather and clear skies cause radiation loss from the ground, sending temperatures down to .

The climate of the area is coastal desert, similar to La Pampa, which is influenced by the dry climate and the Humboldt Current. It is characterized by abundant cloudiness, and low oscillation amplitude from autumn throughout the winter to the early part of spring. But this changes in summer when temperatures double and the oscillation increases, and temperature can vary considerably throughout the day. In the morning it may be sunny, but be very cloudy or rainy in the afternoon.

Often patients with Cockayne Syndrome will severely burn or blister with very little heat exposure. The eyes of patients can be affected in various ways and eye abnormalities are common in CS. Cataracts and cloudiness of the cornea (corneal opacity) are common. The loss of and damage to nerves of the optic nerve, causing optic atrophy can occur. Nystagmus, or involuntary eye movement, and pupils that fail to dilate demonstrate a loss of control of voluntary and involuntary muscle movement.

Changes of 3–4% in cloudiness and concurrent changes in cloud top temperatures correlated to the 11 and 22-year solar (sunspot) cycles, with increased GCR levels during "antiparallel" cycles. Global average cloud cover change was measured at 1.5–2%. Several GCR and cloud cover studies found positive correlation at latitudes greater than 50° and negative correlation at lower latitudes. However, not all scientists accept this correlation as statistically significant, and some who do attribute it to other solar variability (e.g.

The Iwonicz forests create a microclimate around the resort, regulating humidity and temperature of the air, protecting it from winds and are a source of ozone. The resort is situated in the area of the greatest insolation and lowest cloudiness in Poland, which, all-in-all makes it a perfect spot for soothing, refreshing and regenerating the body. The greatest wealth of Iwonicz land are mineral waters and moor mud, which are natural curative agents. These are chloride-bicarbonate-sodium, fluoride, iodide, boric and bromide waters.

The disturbance that was to become Tropical Storm Yunya was first mentioned on July 16 by the Joint Typhoon Warning Center when it was located in the South China Sea as cloudiness in a reverse-oriented monsoon trough. A weak low-level circulation was identified through animated satellite imagery and synoptic data early that morning. Moving east-northeast, the system strengthened into Tropical Depression 11W by July 18. At 0600 UTC that day, the Japan Meteorological Agency declared the formation of Tropical Storm Yunya.

Beatriz moved northwest, due to influence from the outflow from the developing Tropical Storm Arlene in the Gulf of Mexico, briefly reaching its peak intensity of 65 mph (105 km/h) on June 19, shortly prior to landfall near Puerto Escondido, Oaxaca. The storm quickly made its landfall in Puerto Escondido, Oaxaca. Beatriz rapidly weakened after landfall, dissipating over the mountainous southwest Mexican terrain, although the remnant cloudiness associated from the storm's circulation spread over portions of the western Gulf of Mexico on June 20.

Hurricane Katrina was a late-forming tropical cyclone that impacted portions of the Greater Antilles and Bahamas in November 1981\. The twenty-first tropical cyclone, eleventh named storm, and seventh hurricane of the 1981 Atlantic hurricane season, Katrina developed from an area of cloudiness in the western Caribbean Sea early on November 3\. The initial tropical depression deepened slowly, and was upgraded to Tropical Storm Katrina on November 5\. About six hours later, Katrina peaked with sustained winds of 85 mph (140 km/h).

A marine layer can also be driven away by sufficiently strong winds. It is not unusual to hear media weather reporters discuss the marine layer as if it were synonymous with the fog or stratus it may contain, but this is erroneous. In fact, a marine layer can exist with virtually no cloudiness of any kind, although it usually does contain some. The marine layer is a medium within which clouds may form under the right conditions; it is not the layers of clouds themselves.

Secondary to deforestation, groundwater pollution, and climate change, São Paulo is increasingly susceptible to drought and water shortages. People's Park Due to the altitude of the city, there are only few hot nights in São Paulo even in the summer months, with minimum temperatures rarely exceeding . In winter, however, the strong inflow of cold fronts accompanied by excessive cloudiness and polar air cause very low temperatures, even in the afternoon. Afternoons with maximum temperatures ranging between are common even during the fall and early spring.

Ackerman, p. 124 As difficult as it is to evaluate the influences of current clouds on current climate, it is even more problematic to predict changes in cloud patterns and properties in a future, warmer climate, and the resultant cloud influences on future climate. In a warmer climate more water would enter the atmosphere by evaporation at the surface; as clouds are formed from water vapor, cloudiness would be expected to increase. But in a warmer climate, higher temperatures would tend to evaporate clouds.

This process is performed mechanically closed environment by application of automation controls without implementing any chemical treatment and natural mineral content of the water is fully preserved. Water produced in the pants meets the standards accepted by the World Health Organization as well as other international organizations. Some quality indicators of water processed in the filters (chlorine residue, cloudiness, pH, TOC) are controlled online. More parameters of raw and treated water are studied and quality indicators are fully controlled in the laboratory of the complex.

In the Southern Hemisphere, they have been documented to occur between June and November. Cold air damming events which occur when the parent surface high-pressure system is relatively weak, with a central pressure below , or remaining a progressive feature (move consistently eastward), can be significantly enhanced by cloudiness and precipitation itself. Clouds and precipitation act to increase sea level pressure in the area by 1.5 to 2.0 mb ( 0.04 to 0.06 inHg). When the surface high moves offshore, the precipitation itself can cause the CAD event.

Satellite image based largely on observations from NASA's Moderate Resolution Imaging Spectroradiometer (MODIS) on July 11, 2005 of Earth's cloud cover. Cloud cover (also known as cloudiness, cloudage, or cloud amount) refers to the fraction of the sky obscured by clouds when observed from a particular location. Okta is the usual unit of measurement of the cloud cover. The cloud cover is correlated to the sunshine duration as the least cloudy locales are the sunniest ones while the cloudiest areas are the least sunny places.

Binghamton is the 10th rainiest city in the United States, with 162 rainy days a year. With 212 cloudy days annually, it is also the seventh cloudiest city in the country, and the cloudiest east of the Rocky Mountains. Binghamton's proximity to the Great Lakes results in significant cloudiness and precipitation, as weather systems traveling over the lake pick up significant moisture, and cooler air masses from the west and the north culminate in a continuously unsettled weather pattern. Snowfall is significant, with an annual total of .

The cloudiness and thunderstorms became more consolidated off the coast of southern Mexico, and on July 31 Dvorak classifications began on the system. A circulation developed, and the system organized into Tropical Depression Six-E on August 1 while located about 520 mi (835 km) south of the southern tip of Baja California Peninsula. Initially, the depression was a small system with moderate amounts of easterly wind shear. It organized slowly, and after moving to the southwest for 24 hours it turned to the northwest.

The following is a list of cities by sunshine duration. Sunshine duration is a climatological indicator, measuring duration of sunshine in given period (usually, a day or a year) for a given location on Earth, typically expressed as an averaged value over several years. It is a general indicator of cloudiness of a location, and thus differs from insolation, which measures the total energy delivered by sunlight over a given period. Sunshine duration is usually expressed in hours per year, or in (average) hours per day.

Despite the shear, the storm maintained a well-defined wind circulation for several days, with intermittent bursts of thunderstorms near its center. By July 22, Bret had been devoid of strong thunderstorm activity for several hours, prompting the National Hurricane Center to discontinue public advisories when it was located about 375 miles (605 km) north of Bermuda. Since Bret remained over the open Atlantic for most of its existence, its effects on land were limited. While moving little, the storm produced inclement weather and widespread cloudiness over much of the north-central Bahamas.

Negative and positive iodoform test This reaction forms the basis of the iodoform test which was commonly used in history as a chemical test to determine the presence of a methyl ketone, or a secondary alcohol oxidizable to a methyl ketone. When iodine and sodium hydroxide are used as the reagents a positive reaction gives iodoform, which is a solid at room temperature and tends to precipitate out of solution causing a distinctive cloudiness. In organic chemistry, this reaction may be used to convert a terminal methyl ketone into the analogous carboxylic acid.

The purpose of disinfection in the treatment of waste water is to substantially reduce the number of microorganisms in the water to be discharged back into the environment for the later use of drinking, bathing, irrigation, etc. The effectiveness of disinfection depends on the quality of the water being treated (e.g., cloudiness, pH, etc.), the type of disinfection being used, the disinfectant dosage (concentration and time), and other environmental variables. Cloudy water will be treated less successfully, since solid matter can shield organisms, especially from ultraviolet light or if contact times are low.

The winter in Seoul is controlled by the large Siberian high pressure system (the Asiatic high), which results in predominantly cold, dry north-westerly winds. The influence of the Siberian high leads to significantly colder winter temperatures than would be expected at this latitude. About every 4 to 6 days a low-pressure trough will move through South Korea, bringing with it cloudiness and light precipitation. The amount of precipitation locally depends mostly on the elevation of the station and the length of time that the air has been over the Yellow Sea.

Lisch epithelial corneal dystrophy is characterized by feather shaped opacities and microcysts in the corneal epithelium that are arranged in a band-shaped and sometimes whorled pattern. Painless blurred vision sometimes begins after sixty years of life. Corneal stromal dystrophies - Macular corneal dystrophy is manifested by a progressive dense cloudiness of the entire corneal stroma that usually first appears during adolescence and eventually causing severe visual impairment. In Granular corneal dystrophy multiple small white discrete irregular spots that resemble bread crumbs or snowflakes become apparent beneath Bowman zone in the superficial central corneal stroma.

In the lower reaches, there is a large flux in particulate material and also a decrease in production through photosynthesis, due to an increase in water cloudiness (turbidity) and surface film from suspended FPOM. Here, like the headwaters, respiration outpaces photosynthesis, making the ratio again less than 1 (P: R <1). The living community in these areas are made up of almost exclusively collectors, as well as a small share of predators.Stout III, Ben M. "River Continuum Concept as Analytical Template for Assessing Watershed Health" Wheeling Jesuit University. 2003.

Low-pressure systems, also known as cyclones, are located in minima in the pressure field. Rotation is inward at the surface and counterclockwise in the northern hemisphere as opposed to inward and clockwise in the southern hemisphere due to the Coriolis force. Weather is normally unsettled in the vicinity of a cyclone, with increased cloudiness, increased winds, increased temperatures, and upward motion in the atmosphere, which leads to an increased chance of precipitation. Polar lows can form over relatively mild ocean waters when cold air sweeps in from the ice cap.

Cloudiness – Skies are heavily clouded during the monsoon months and for short spells when the region is affected by the passage of western disturbances. During the rest of the year the skies are generally clear to lightly clouded. Winds – Owing to the nature of terrain local affect are pronounced and when the general prevailing winds not too strong to mask these effect, there is a tendency for diurnal reversal of winds, the flow being anabatic during the day and katabatic at night, the latter being of considerable force.

Their formation can also be triggered by changes in air pressure in wingtip vortices or in the air over the entire wing surface. Contrails, and other clouds directly resulting from human activity, are collectively named homogenitus. Depending on the temperature and humidity at the altitude the contrails form, they may be visible for only a few seconds or minutes, or may persist for hours and spread to be several miles wide, eventually resembling natural cirrus or altocumulus clouds. Persistent contrails are of particular interest to scientists because they increase the cloudiness of the atmosphere.

Like the rest of the Willamette Valley, Corvallis falls within the dry-summer temperate climate zone, also referred to as cool-summer Mediterranean (Köppen Csb). Temperatures are mild year round, with warm, dry, sunny summers and mild, wet winters with persistently overcast skies. Spring and fall are also moist seasons with varied cloudiness, and light rain falling for extended periods. Winter snow is rare, but occasionally does fall, and amounts can range between a dusting and a few inches that do not persist on the ground for more than a day.

The higher albedos for snow and ice cause rapid shifts in surface reflectivity in autumn and spring in high latitudes, but the overall climatic significance of this increase is spatially and temporally modulated by cloud cover. (Planetary albedo is determined principally by cloud cover, and by the small amount of total solar radiation received in high latitudes during winter months.) Summer and autumn are times of high-average cloudiness over the Arctic Ocean so the albedo feedback associated with the large seasonal changes in sea-ice extent is greatly reduced.

Changes in subtropical humidity could provide a negative feedback that decreases the amount of water vapor which in turn would act to mediate global climate transitions. Changes in cloud cover are closely coupled with other feedback, including the water vapor feedback and ice-albedo feedback. Changing climate is expected to alter the relationship between cloud ice and supercooled cloud water, which in turn would influence the microphysics of the cloud which would result in changes in the radiative properties of the cloud. Climate models suggest that a warming will increase fractional cloudiness.

In terms of the test itself, the kauri-butanol value (Kb) of a chemical shows the maximum amount of the hydrocarbon that can be added to a solution of kauri resin (a thick, gum-like material) in butanol (butyl alcohol) without causing cloudiness. Since kauri resin is readily soluble in butyl alcohol but not in most hydrocarbon solvents, the resin solution will tolerate only a certain amount of dilution. "Stronger" solvents such as benzene can be added in a greater amount (and thus have a higher Kb value) than "weaker" solvents like mineral spirits.

On August 28, an area of convectional cloudiness associated with a monsoon trough formed about southwest of Okinawa, Japan. Satellite imagery revealed that a partial low-level circulation centre (LLCC) was exposed with an anticyclone providing good outflow that located to the northwest of the system. Early on September 1, the system showed a more defined LLCC moving through warm waters, whilst JMA upgraded the system to a tropical depression. On September 2, the depression entered the Philippine area of responsibility and PAGASA assigned it a local name Labuyo.

On September 6, an area of convection cloudiness associated with the monsoon through was formed about to the northwest of Manila, Philippines. Satellite imagery shows that a mid-level convection consolidating in over a developing Low-Level Circulation Centre (LLCC). In additionally, there is a westerly wind burst that located three to five degrees of the system and located in moderate vertical wind shear. Late of September 8, the system is moving northwest and also in hot water temperatures, whilst the JMA upgraded the system into a tropical depression.

On September 9, an area of convectional cloudiness associated with the monsoon trough formed to the northwest of Palau. Satellite imagery showed that a consolidating Low Level Circulation Centre (LLCC) with convection had started to develop and was wrapping toward the center. On September 11, the LLCC started to show improvement and was under moderate vertical shear with good westward outflow, but the JMA still upgraded the system to a minor tropical depression. Early of September 12, PAGASA upgraded the system in their responsibility and assigned its local name, Nando.

On October 6, an area of convectional cloudiness associated with the monsoon trough formed to the southwest of Saipan. Satellite imagery showed a consolidating Low Level Circulation Center with formative convective banding and deep convection over the northern semicircle. During the morning of October 8, the system started to move northwest and its LLCC rapidly became well defined due to favorable conditions. The JMA then upgraded it to a tropical depression, and the JTWC issued a TCFA on the system, as it had started to become better defined.

The shape of the central dense overcast is also considered. The farther the center is tucked into the CDO, the stronger it is deemed. Tropical cyclones with maximum sustained winds between and can have their center of circulations obscured by cloudiness within visible and infrared satellite imagery, which makes diagnosis of their intensity a challenge. The CCC pattern, with its large and quickly developing mass of thick cirrus clouds spreading out from an area of convection near a tropical cyclone center within a short time frame, indicates little development.

Because of their delicate dependency on local climates, cloud forests will be strongly affected by global climate change. Results show that the extent of environmentally suitable areas for cloud forest in Mexico will sharply decline in the next 70 years. A number of climate models suggest low-altitude cloudiness will be reduced, which means the optimum climate for many cloud forest habitats will increase in altitude. Linked to the reduction of cloud moisture immersion and increasing temperature, the hydrological cycle will change, so the system will dry out.

On June 14, satellite imagery revealed an increase in thunderstorm activity to the south of the Gulf of Tehuanpec. Moving little, a broad surface low developed with the cloud mass, and a tropical wave moved through the area. Although the disturbance remained disorganized, a second tropical wave moved into the region on June 18, when the cloudiness there became better concentrated. According to a post-storm analysis of satellite data and synoptic reports, it is noted that a tropical depression formed at 0600 UTC on June 18, while located approximately south- southeast of Huatulco, Mexico.

A tropical wave moved off the western coast of Africa on June 23, and for the next two weeks, moved through the tropical waters of the Atlantic Ocean and later crossed Central America. It began developing further when it entered the Pacific Ocean and became a dense area of moisture and cloudiness. The wave developed into a disturbance on July 8, and attained tropical depression status in the afternoon on July 8, south of Mexico. After entering a favorable area of warm waters, the depression strengthened to Tropical Storm Carlotta on July 9.

Light fog in the southern valley The climate of the Willamette Valley is a mix of Mediterranean (Köppen Csb) and oceanic (Köppen Cfb) influences. The Köppen climate classification system considers it Mediterranean, but compared to a true Mediterranean climate it is cooler and moister, with a longer rainy season. The main climatic features are moderate temperatures and frequent cloudiness and rains, except in summer when the northward expansion of the North Pacific High creates generally sunny and warm weather. Winters are consistently wet and cloudy, and often foggy, but quite mild.

Most of the rainfall during summer and fall is caused by convective thunderstorms. Winter (June–August) is the driest season, with a mean precipitation of throughout the region. Most of the winter precipitation is the result of synoptic scale, low pressure weather systems (large scale storms such as extratropical cyclones), particularly the sudestada, which often bring long periods of precipitation, cloudiness, cooler temperatures, and strong winds. Snowfall is extremely rare and mainly confined to the uplands of Misiones Province where the last significant snowfall occurred in 1975 in Bernardo de Irigoyen.

Places in the east receive rainfall throughout autumn, whereas in the west it quickly becomes very dry. Winters are drier in most places due to weaker easterly winds, and stronger southerly winds, which prevent moist air from coming in. In winter, most of the precipitation occurs from frontal systems associated with cyclogenesis and strong southeasterly winds (sudestada), which bring long periods of precipitation, and cloudiness, particularly in the southern and eastern parts. As such, precipitation is more evenly distributed in the eastern parts than the western parts, which are further away from these frontal systems.

January to March are the wettest months with the advance of Atlantic tropical masses, and the months from June to August are the driest, due to the influence of the polar mass, but with relatively high precipitation. Sunshine hours are a bit low for the subtropics, being part of the effect of the large amount of water vapor on the airand the consequent cloudiness present. Collaborating with the high humidity, the prevailing winds come from the east, especially in the ENE. Winds over 19 km/h are rare and more favorable in September.

The most common causes of such turbulence are strong upper level low pressure areas, or the monsoon which occasionally extends northwestward from the desert areas of the U.S. There are also occasional extended spells when fog and stratus ("overcast") do not clear all the way back to the coast for several days. These extended periods of cloudiness are usually a consequence of a weak area of low pressure above the marine layer which increases its depth, making it more difficult for surface heating to evaporate the clouds within it.

The climate of the colony can be classified as tropical steppe, semi-arid and hot; the climate is extremely dry except during the monsoon time. During three months of south-west monsoon, usually the last week of June to September, the moist oceanic air penetrates into the colony and causes high humidity, cloudiness, and heavy rainfall. The period from October to December squashes post-monsoon rains. The winter spans from January to the beginning of March and is followed by the summer season which lasts until the last week of June.

The cloudiness can be cleared up by either "cold breaking," which is leaving the mead in a cold environment overnight, or using a fining material, such as sparkolloid, bentonite, egg white, or isinglass. If the mead maker wishes to backsweeten the product or prevent it from oxidizing, potassium metabisulfite and potassium sorbate are added. After the mead clears, it is bottled and distributed. Primary fermentation usually takes 28 to 56 days, after which the must is placed in a secondary fermentation vessel for 6 to 9 months of aging.

On October 30, a poorly-defined tropical wave and its associated small area of disturbed weather emerged into the Atlantic from the west coast of Africa. Strong wind shear prevented significant development or organization of deep convection for a few days. However, by November 5, cloudiness and showers increased as the system was approaching the Lesser Antilles. After a rapid increase in convection and the circulation becoming more well-defined on satellite imagery, a tropical depression about 115 mi (190 km) southeast of San Salvador Island in the Bahamas around 18:00 UTC on November 8\.

In Europe and the Middle East, changes in atmospheric colours, storms, cold, and severe weather were reported in 1258–1259, with agricultural problems extending to North Africa. In Europe, excess rain, cold and high cloudiness damaged crops and caused famines followed by epidemics, although 1258–1259 did not lead to famines as bad as some other famines such as the Great Famine of 1315–17. In northwest Europe, the effects included crop failure, famine, and weather changes. A famine in London has been linked to this event; this food crisis was not extraordinary and there were issues with harvests already before the eruption.

The relatively high latitude of 49° 15′ 0″ N (similar to Paris, France, at 48° 85′ 66″) means sunsets as early as 4:15 pm and sunrises as late as 8:10 am. From November to February, at the sunshine measuring station at the airport in Richmond, on average more than 70% of the already short daytime is completely cloudy. The percentage of cloudiness is higher in Vancouver and especially the North Shore because upslope winds going up the mountainsides lead to the development of clouds. Summers, in contrast, are characterized by a nearly opposite weather pattern, with consistent high pressure and sunshine.

His broad phrasing and the sonority of his voice also allowed him to create characters that were both noble and imposing. Over time Basiola had to make some concessions to verismo vocalism, and his incessant activity did bring about some cloudiness of the voice, but his technique and style made him much in demand, especially in works from the second half of the 19th century. What he could not entirely achieve was to put an unmistakably personal stamp on his interpretations. Nevertheless, Basiola was his immense technical and artistic value during his career and to modern historians of the voice and singing.

An unnamed hurricane in November 1991, and Subtropical Storm Alpha in September 2020 also formed in this manner. After being classified as a hurricane, Karl gradually strengthened, and its circulation became more distinguished from the surrounding cloudiness. A trough that emerged from North America steered the hurricane eastward, and on November 26, it reached its peak intensity with maximum sustained winds of 85 mph (140 km/h) and a central barometric pressure reading of 985 mbar (hPa; 29.09 inHg). Karl maintained this strength for approximately 18 hours until beginning to weaken slightly as it accelerated towards the northeast.

Each blade has its own path around the tun and the whole rake assembly can be raised and lowered. Attached to each of these arms is a flap which can be raised and lowered for pushing the spent grains out of the tun. The brewer, or better yet an automated system, can raise and lower the rake arms depending on the turbidity (cloudiness) of the run-off, and the tightness of the grain bed, as measured by the pressure difference between the top and bottom of the grain bed. There must be a system for introducing sparge water into the lauter tun.

Like most of Labrador, Wabush has a subarctic climate (Köppen Dfc) with precipitation much higher than usual for this type of climate due to the persistent Icelandic Low, which give the region some of the rainiest and snowiest weather in all of Canada. Especially in summer, cloudiness is very high due to the lakes nearby and the unstable northerly airstreams that prevail, but because the town is relatively far from the open sea, sunshine is higher than even in St. John's due to the absence of fog from the Labrador Current. Snow usually melts off in May.

In early June, a strong pulse of the Madden-Julian Oscillation (MJO) tracked eastwards into the tropical Indian Ocean, leading to increased cloudiness and rainfall across the region. On June 9, the India Meteorological Department (IMD) noted the development of a low-pressure area over the southeastern Arabian Sea, to the north of the Maldives. Early on June 10, a depression formed in the Arabian Sea, just northwest of the Maldives, and the IMD gave the storm the identifier ARB 01. As the system moved northward, it gradually strengthened, becoming a deep depression, before intensifying further into Cyclonic Storm Vayu later that day.

A tropical wave moving westward off the African coast on October 1, 2001 entered the tropical Atlantic. The wave's organization changed little until October 4 as it moved westward, when curved banding features began to increase. However, little improvement in the wave's organization occurred until October 6 after continuing to move westward for two days, when an area of low pressure was identified by the National Hurricane Center. Afterward, the cloudiness became more concentrated, and the system organized into a tropical depression by noon on October 6, shortly after the first advisory from the NHC was issued at 11 a.m. AST.

Daytime weather is typically rather mild compared to parts of the country further north or further south. However, due to the city's high elevation, daily temperature differences can vary widely and low temperatures in winter typically dip well below freezing. The daily average temperatures in December and January, the coldest months, are slightly above freezing at and respectively. Albuquerque's climate is usually sunny and dry, with an average of 3,415 sunshine hours per year. Brilliant sunshine defines the region, averaging 278 days a year; periods of variably mid and high-level cloudiness temper the sun, mostly during the cooler months.

Two photo transistors are mounted so they measure a high degree of reflected light when the mirror is clear (direct) and scattered light when the mirror is clouded with visible condensation (indirect). With the formation of condensation on the mirror, the degree of cloudiness of the mirror surface increases with the direct transistor receiving less light and the indirect transistor more light. The output from these photo transistors controls the mirror cooling module which is an electronic heat pump that operates much like a thermocouple in reverse, producing a heating or cooling effect. When the sensor is first activated, the mirror is clear.

On August 27, JMA reported that an area of convectional cloudiness associated with monsoon through formed about , to the southeast of Iwo To, Japan. Satellite imagery shows that convective bands is starting to wrap into the Low-Level Circulation Centre (LLCC) and the system is located in moderate vertical windshear and favorable area. Early of August 28, the system is showing a good development LLCC then the JMA upgraded the system into a minor tropical depression. While JTWC issued a Tropical Cyclone Formation Alert (TCFA) on the system then after several hours, they upgraded it into a tropical depression.

The amount of solar radiation reaching ground level in rugged terrain, or due to variable cloudiness, is parameterized as this process occurs on the molecular scale. This method of parameterization is also done for the surface flux of energy between the ocean and the atmosphere in order to determine realistic sea surface temperatures and type of sea ice found near the ocean's surface. Also, the grid size of the models is large when compared to the actual size and roughness of clouds and topography. Sun angle as well as the impact of multiple cloud layers is taken into account.

Cataract surgery, using a temporal approach phacoemulsification probe (in right hand) and "chopper" (in left hand) being done under operating microscope at a Navy medical center A cataract is an opacification or cloudiness of the eye's crystalline lens due to aging, disease, or trauma that typically prevents light from forming a clear image on the retina. If visual loss is significant, surgical removal of the lens may be warranted, with lost optical power usually replaced with a plastic intraocular lens. Owing to the high prevalence of cataracts, cataract extraction is the most common eye surgery. Rest after surgery is recommended.

The system that would eventually become the series of mid-January winter storms was first noted as an area of disorganized cloudiness to the east of Japan on 10 January. Slowly crossing the north Pacific, the system organized sufficiently to be named Winter Storm Jacob by The Weather Channel on 14 January, while located off the coast of the Pacific Northwest. After undergoing rapid intensification into a strong Pacific Northwest windstorm, Jacob made landfall over Washington state on 15 January. After crossing the northern United States, the system emerged into the north Atlantic on 17 January, crossing the coast of Virginia.

Quickly strengthening, the depression intensified a tropical storm six hours later based on a ship report, earning the name Beatriz. Moving generally towards the northwest, partially due to Tropical Storm Arlene's large circulation in the Gulf of Mexico, Beatriz reached a peak intensity of by 1800 UTC on June 19. Shortly thereafter, the system made landfall near Puerto Escondido, Oaxaca and rapidly weakened to a tropical depression over the mountainous terrain of Mexico. Beatriz dissipated at 0600 UTC on June 20, although the remnant cloudiness and associated convection from the storm spread across portions of the western Gulf of Mexico that same day.

AccuWeather created a unified and proprietary apparent temperature system known as "The AccuWeather Exclusive RealFeel Temperature" and has used the quantity in its forecasts and observations. The formula for calculating this value incorporates the effects of temperature, wind, humidity, sunshine intensity, cloudiness, precipitation, and elevation on the human body, similar to the rarely used (but public domain) wet-bulb globe temperature. AccuWeather has been granted a United States patent on The RealFeel Temperature, but the formula is a trade secret and has not been reviewed by other meteorological authorities. In response to AccuWeather's "RealFeel", The Weather Channel introduced their "FeelsLike" temperature reading.

During its formative stages, the precursor disturbance interacted with the monsoon trough to produce widespread cloudiness over Panama in the first week of October. Flooding rains fell over much of the Talamanca and Central mountain ranges, including the west-central provinces of Chiriquí, Ngäbe-Buglé, Veraguas, Panamá Oeste, Bocas del Toro, and Coclé, as well as Colón and Guna Yala along the Atlantic coast. On October 3, Panamanian officials issued an alert for heavy rain with strong gusts and urged residents on the riverbanks of Río de Jesús to evacuate. In Ngäbe-Buglé, a landslide killed six people.

Within the basin, most tropical cyclones have their origins within the South Pacific Convergence Zone or within the Northern Australian monsoon trough, both of which form an extensive area of cloudiness and are dominant features of the season. Within this region a tropical disturbance is classified as a tropical cyclone, when it has 10-minute sustained wind speeds of more than 65 km/h (35 mph), that wrap halfway around the low level circulation centre, while a severe tropical cyclone is classified when the maximum 10-minute sustained wind speeds are greater than 120 km/h (75 mph).

The anatomy of finless porpoises has been relatively well studied, compared with that of some other cetacean species. The tubercles along the dorsal ridge are known to contain numerous nerve endings is used as a sensory function. The auditory system also appears well-developed, with numerous nerve fibres specialised for rapid communication between the ears and the brain. Sight is relatively poor, however, due to the overall cloudiness of the Yangtze River; they have a reduced lens and a limited number of fibres in the optic nerve and to the muscles moving the eyes compared to the Indo-pacific finless porpoise.

Cloudiness A foggy day in Hyderabad June to October is the period when more than half of the sky is covered with clouds, while only about a quarter of the sky is clouded from January to March. Half of the days in July and August have overcast skies. About 10 to 13 days in the months of January, February and March, the skies are free from clouds in clear weather. Recent Temperature Increases According to India Meteorological Department, the summer months of April and May 2009 recorded the warmest temperatures since 1901, with mean maximum temperatures hovering frequently at around 42 °C with maximum temperature touching 45 °C.

The last times it snowed in Valdivia were in July 2007 and in August 1995 during the so-called Terremoto Blanco (Spanish for White Earthquake). The Seven Lakes in the interior help to keep an average relative humidity of 80% for the region as whole and there are no months with less than 75% average humidity. The precipitation is generated by frontal systems that cross the zone, which produce cloudiness and few clear days. The leeward effect of the Valdivian Coast Range is minimal due to its low height (715 m at Cerro Oncol) and the gap in the range at Valdivia River's outflow to the Pacific Ocean.

Depictions of the Bodhisattvas Ksitigarbha and Avalokiteshvara sometimes show them holding this Cintamani, indicating their ability to fulfill the wishes of sentient beings. The Mani Jewel also appears as a water purifying jewel (清水摩尼) where it could be placed in muddy water by traveling monks, causing any cloudiness to settle out leaving the water clear and pure. This version of the jewel is mentioned in the Abhidharma-kosa where it is used as a metaphor for faith as an agent capable of dispelling uncertainty. Yet another depiction of the jewel is in the metaphor of Indra's net which appears in the Avatamsaka Sutra.

March brings more frequent frost, but also nice stretches of sunny weather. The average high temperature is 19 °C, the low is 4 °C, occasionally 30 °C can be reached, and temperatures may fall to -5 °C. The most radical change occurs sometime during the month of April, when Villa La Angostura first gets in the path of a "train of Pacific storms": in the end, total precipitation for the month averages . The average high is 14 °C (57 F), the low is 2 °C or 35 F(the nighttime change is small due to increased cloudiness)and by late April any cloudless night will be frosty.

In early June, a strong pulse of the Madden-Julian Oscillation (MJO) tracked eastwards into the tropical Indian Ocean, leading to increased cloudiness and rainfall across the region. The presence of the pulse also contributed to enhanced convective activity, and generated conditions which were supportive of tropical cyclogenesis. On 9 June, the India Meteorological Department (IMD) noted the development of a low-pressure area over the southeastern Arabian Sea, to the north of the Maldives. Organisation increased throughout the day, and owing to the improved structure of the system, the United States' Joint Typhoon Warning Center (JTWC) issued a tropical cyclone formation alert at 22:30 UTC.

Cloud feedback is the coupling between cloudiness and surface air temperature where a surface air temperature change leads to a change in clouds, which could then amplify or diminish the initial temperature perturbation. Cloud feedbacks can affect the magnitude of internally generated climate variability or they can affect the magnitude of climate change resulting from external radiative forcings. Global warming is expected to change the distribution and type of clouds. Seen from below, clouds emit infrared radiation back to the surface, and so exert a warming effect; seen from above, clouds reflect sunlight and emit infrared radiation to space, and so exert a cooling effect.

The Arctic Basin is typically covered by sea ice year round, which strongly influences its summer temperatures. It also experiences the longest period without sunlight of any part of the Arctic, and the longest period of continuous sunlight, though the frequent cloudiness in summer reduces the importance of this solar radiation. Despite its location centered on the North Pole, and the long period of darkness this brings, this is not the coldest part of the Arctic. In winter, the heat transferred from the water through cracks in the ice and areas of open water helps to moderate the climate some, keeping average winter temperatures around .

As the equatorward portion of the system approaches the cold air wedge, persistent low cloudiness, such as stratus, and precipitation such as drizzle develop, which can linger for long periods of time; as long as ten days. The precipitation itself can create or enhance a damming signature, if the poleward high is relatively weak. If such events accelerate through mountain passes, dangerously accelerated mountain-gap winds can result, such as the Tehuantepecer and Santa Ana winds. These events are seen commonly in the northern Hemisphere across central and eastern North America, south of the Alps in Italy, and near Taiwan and Korea in Asia.

Rock sandpiper Saint Paul's climate is strongly influenced by the cold waters of the surrounding Bering Sea, and is classified as polar (Köppen ET) due to the raw chilliness of the summers. It experiences a relatively narrow range of temperatures, high wind, humidity and cloudiness levels, and persistent summer fog. There is high seasonal lag: February is the island's coldest month, while August is its warmest; the difference between the average low temperature in February and the average high temperature in August is only . Although the mean average temperature for the year is above freezing, at , the monthly daily average temperature remains below freezing from December to April.

Sunshine duration or sunshine hours is a climatological indicator, measuring duration of sunshine in given period (usually, a day or a year) for a given location on Earth, typically expressed as an averaged value over several years. It is a general indicator of cloudiness of a location, and thus differs from insolation, which measures the total energy delivered by sunlight over a given period. Sunshine duration is usually expressed in hours per year, or in (average) hours per day. The first measure indicates the general sunniness of a location compared with other places, while the latter allows for comparison of sunshine in various seasons in the same location.

A weakly defined tropical wave moved off the northwest coast of Africa on September 20, and crossed the northern portion of the tropical Atlantic and northern South America without significant organization. The wave moved into the northeastern Pacific waters, off the coast of Colombia on September 30. As the wave passed over southern Central America, rainbands and cloudiness increased with the system between October 1 and October 3, before the system merged with the ITCZ from October 4 to October 6. Signs of convective organization reappeared on October 8, and by October 9, the system was upgraded to Tropical Depression Twenty Two-E south of Cabo San Lucas, Mexico.

Still, sub grid scale processes need to be taken into account. Rather than assuming that clouds form at 100% relative humidity, the cloud fraction can be related to a critical relative humidity of 70% for stratus-type clouds, and at or above 80% for cumuliform clouds, reflecting the sub grid scale variation that would occur in the real world. The amount of solar radiation reaching ground level in rugged terrain, or due to variable cloudiness, is parameterized as this process occurs on the molecular scale. Also, the grid size of the models is large when compared to the actual size and roughness of clouds and topography.

Typhoon Chan-hom, known in the Philippines as Typhoon Emong, is the sixth tropical depression and the second tropical storm to develop during the 2009 Pacific typhoon season. Chan-hom developed out of an area of convectional cloudiness associated with an area of disturbed weather which originated from the remnants of Tropical Depression Crising and formed southeast of Nha Trang, Vietnam on May 2. Moving towards the northeast, it slowly organized according to JTWC who issued a TCFA, and JMA classified Chan-hom as a minor tropical depression later that day. The next day, both JTWC and JMA upgraded the depression to a tropical storm and named it Chan-hom.

Typhoon Nancy originated from a large area of convection situated in the middle of the Pacific Ocean, which, while drifting westward, began to consolidate on October 8 within a favorable environment aloft. The convection separated from an upper-level low embedded within a tropical upper- tropospheric trough (TUTT). Later that day, the area of convection degenerated into a "random area of cloudiness." The TUTT drifted west while the Joint Typhoon Warning Center (JTWC) reported that a tropical depression formed within the area of convection that was now located south of the TUTT. Early on October 10, the Japan Meteorological Agency (JMA) started watching the system.

On land, terrain maps available at resolutions down to globally are used to help model atmospheric circulations within regions of rugged topography, in order to better depict features such as downslope winds, mountain waves and related cloudiness that affects incoming solar radiation. The main inputs from country-based weather services are observations from devices (called radiosondes) in weather balloons that measure various atmospheric parameters and transmits them to a fixed receiver, as well as from weather satellites. The World Meteorological Organization acts to standardize the instrumentation, observing practices and timing of these observations worldwide. Stations either report hourly in METAR reports, or every six hours in SYNOP reports.

In mid-June, a broad cyclonic area of cloudiness persisted to the south of the Gulf of Tehuantepec. A low-level circulation and banding features became more prominent on June 16, and further development was aided by the presence of a tropical wave that first departed the western coastline of Africa on June 5\. As extremely deep convection festered within a band west of the disturbance's center, it is estimated the first tropical depression of the season formed around 06:00 UTC on June 18, located about 260 mi (420 km) southeast of Acapulco, Mexico. The newly-formed cyclone tracked west-northwest parallel to the coastline, steered by a strong area of high pressure to its north and east.

The cornflower blue color of the Yogo results from trace amounts of iron and titanium. Yogo sapphires are unique in that they are free of cavities and inclusions, have high uniform clarity, lack color zoning, and do not need heat treating because their cornflower blue coloring is uniform and deep. Unlike Asian sapphires, they maintain their brilliance in artificial light. Yogo sapphires present an advantage to gemcutters: since they are found as primary constituent minerals within an igneous bedrock rather than in sedimentary alluvial deposits where most other sapphires are located, they retain a perfect or near perfect crystalline shape, making cutting much easier, as does their lack of inclusions, color zoning, or cloudiness.

Use of advanced very high resolution infrared satellite imagery can be used, in the absence of cloudiness, to detect density discontinuities (weather fronts) such as cold fronts at ground level. Using the Dvorak technique, infrared satellite imagery can be used to determine the temperature difference between the eye and the cloud top temperature of the central dense overcast of mature tropical cyclones to estimate their maximum sustained winds and their minimum central pressures. Along Track Scanning Radiometers aboard weather satellites are able to detect wildfires, which show up at night as pixels with a greater temperature than . The Moderate- Resolution Imaging Spectroradiometer aboard the Terra satellite can detect thermal hot spots associated with wildfires, volcanoes, and industrial hot spots.

Buckeye has a hot desert climate (Köppen BWh), with abundant sunshine due to the stable descending air of the eastern side of the subtropical anticyclone aloft and at sea level over the southwestern United States. Summers, as with most of the Sonoran Desert, are extremely hot, with 121.0 afternoons reaching and 181.6 afternoons reaching . The record high temperature of occurred on July 28, 1995, and temperatures above may occur in any month. Cooler weather may occasionally occur during summer, but such periods are no less unpleasant as they result from monsoonal weather, with its attendant higher cloudiness and humidity; however, actual rainfall from the monsoon is much more infrequent than in Flagstaff, Nogales or even Tucson.

To facilitate efficient sterilization by steam and pressure, there are several methods of verification and indication used; these include color-changing indicator tapes and biological indicators. When using biological indicators, samples containing spores of heat-resistant microbes such as Geobacillus stearothermophilis are sterilized alongside a standard load, and are then incubated in sterile media (often contained within the sample in a glass ampule to be broken after sterilization). A color change in the media (indicating acid production by bacteria; requires the medium to be formulated for this purpose), or the appearance of turbidity (cloudiness indicating light scattering by bacterial cells) indicates that sterilization was not achieved and the sterilization cycle may need revision or improvement.

In manual systems, the bottles are visually examined for indicators of microbial growth, which might include cloudiness, the production of gas, the presence of visible microbial colonies, or a change in colour from the digestion of blood, which is called hemolysis. Some manual blood culture systems indicate growth using a compartment that fills with fluid when gases are produced, or a miniature agar plate which is periodically inoculated by tipping the bottle.Mahon, CR et al. (2018). pp. 871–2. To ensure that positive blood cultures are not missed, a sample from the bottle is often inoculated onto an agar plate (subcultured) at the end of the incubation period regardless of whether or not indicators of growth are observed.

On July 16, the NHC highlighted the expected formation of an area of low pressure south of Mexico later that week. A tropical wave began producing disorganized cloudiness three days later, and the broad system slowly organized into a tropical depression by 15:00 UTC on July 22. Its structure changed little after formation, impinged by strong wind shear; despite this, satellite wind data indicated the cyclone intensified into Tropical Storm Irwin by 09:00 UTC on July 23. Over the next 24 hours, deep convection began to wrap around the center and a mid-level eye formed as environmental conditions improved; by 09:00 UTC on July 25, Irwin intensified into a hurricane.

SOS works to minimize development near these creeks, as sewage, run-off from roads and lawn fertilizers can end up in the Aquifer and come up at Barton Springs. Some of the ill effects of this pollution include a sewage smell, eutrophication (the proliferation of algae due to increased nutrients), increase turbidity (cloudiness) and harm to endangered species. Barton Creek and other lakes and rivers in Central Texas are very popular in the Austin and Edwards Aquifer region as most citizens enjoy kayaking, swimming, and other outdoor recreation. Pursuant to Section 11(g) of the Endangered Species Act, Save Our Springs Alliance petitioned the Secretary of the Interior to list the Barton Springs Salamander as an endangered species.

Near the equator, increased cloudiness is due to the presence of the low-pressure Intertropical Convergence Zone (ITCZ) where very warm and unstable air promotes mostly cumuliform and cumulonimbiform clouds. Clouds of virtually any type can form along the mid-latitude convergence zones depending on the stability and moisture content of the air. These extratropical convergence zones are occupied by the polar fronts where air masses of polar origin meet and clash with those of tropical or subtropical origin. This leads to the formation of weather-making extratropical cyclones composed of cloud systems that may be stable or unstable to varying degrees according to the stability characteristics of the various airmasses that are in conflict.

In leeward areas well screened from the trade winds (such as the west coast of Maui), skies are clear 30 to 60 percent of the time. Windward areas tend to be cloudier during the summer, when the trade winds and associated clouds are more prevalent, while leeward areas, which are less affected by cloudy conditions associated with trade wind cloudiness, tend to be cloudier during the winter, when storm fronts pass through more frequently. On Maui, the cloudiest zones are at and just below the summits of the mountains, and at elevations of on the windward sides of Haleakala. In these locations the sky is cloudy more than 70 percent of the time.

Widespread cloudiness preceded the event, leading to very little in the way of surface heating with CAPE values generally less than 1000 J/kg. However, given the extremely intense wind fields and favorable mid and upper level support for rising motion, these relatively low levels of instability were more than sufficient for severe thunderstorms and tornadoes. The National Weather Service in New Orleans launched a special sounding at noon on the 23rd that shows both sufficient instability and very strong wind shear. This environment advected across the National Weather Service in Mobile, Alabama area of responsibility during the afternoon and evening and is generally representative of conditions in which the severe thunderstorms formed.

Acute otitis media in children with moderate to severe bulging of the tympanic membrane or new onset of otorrhea (drainage) is not due to external otitis. Also, the diagnosis may be made in children who have mild bulging of the ear drum and recent onset of ear pain (less than 48 hours) or intense erythema (redness) of the ear drum. To confirm the diagnosis, middle-ear effusion and inflammation of the eardrum have to be identified; signs of these are fullness, bulging, cloudiness and redness of the eardrum. It is important to attempt to differentiate between acute otitis media and otitis media with effusion (OME), as antibiotics are not recommended for OME.

Neuberger analysed 12,000 paintings, held in American and European museums and dated between 1400 and 1967, for cloudiness and darkness. His 1970 publication shows an increase in such depictions that corresponds to the Little Ice Age, peaking between 1600 and 1649. Paintings and contemporary records in Scotland demonstrate that curling and ice skating were popular outdoor winter sports, with curling dating back to the 16th century and becoming widely popular in the mid-19th century. As an example, an outdoor curling pond constructed in Gourock in the 1860s remained in use for almost a century, but increasing use of indoor facilities, problems of vandalism, and milder winters led to the pond being abandoned in 1963.

Thunderstorms are common and can bring heavy rain and much cooler weather. As in the entire Pampas region, summers are "cut" by short, cool periods when southerly Pampero winds blow. March is already noticeably cooler than the summer, and April is characterized by very pleasant weather: highs range from 21 °C (70F) to 25 °C (77F), nights from 10 °C (50F) to 14 °C (57F), and May is already generally cool, with chilly nights. Winter runs from late May to late August. Temperatures usually range from 13 °C (55F) to 18 °C (64F), while nights go from 3 °C (37F) to 7 °C (45F), with lower precipitation but higher cloudiness and relatively common fog.

The sea reaches its lowest temperature in February or early March so that on average February is the coldest month in some coastal parts of South Ayrshire along with the Rinns of Galloway, Kintyre and the Hebrides. In February the mean daily minimum temperature varies from about 2 °C in most of the islands, 1 to 2 °C along most of the Solway Firth and lowland inland areas, but less than −1 °C in parts of the Southern Uplands and central Highlands. Inland, where the influence of the sea is less, January is the coldest month with mean daily minimum temperatures generally between −3 and 0 °C. The number of hours of natural sunshine in South Ayrshire is controlled by the length of day and by cloudiness.

Once a cyclone occludes an occluded front (a trough of warm air aloft) will be caused by strong southerly winds on its eastern periphery rotating aloft around its northeast, and ultimately northwestern, periphery (also termed the warm conveyor belt), forcing a surface trough to continue into the cold sector on a similar curve to the occluded front. The front creates the portion of an occluded cyclone known as its comma head, due to the comma-like shape of the mid-tropospheric cloudiness that accompanies the feature. It can also be the focus of locally heavy precipitation, with thunderstorms possible if the atmosphere along the front is unstable enough for convection. Banding within the comma head precipitation pattern of an extratropical cyclone can yield significant amounts of rain.

Irritancy can be measured using the Draize test, where a test substance is applied to an animal's eyes or skin, usually an albino rabbit. For Draize eye testing, the test involves observing the effects of the substance at intervals and grading any damage or irritation, but the test should be halted and the animal killed if it shows "continuing signs of severe pain or distress". The Humane Society of the United States writes that the procedure can cause redness, ulceration, hemorrhaging, cloudiness, or even blindness.Species Used in Research: Rabbit, Humane Society of the United States This test has also been criticized by scientists for being cruel and inaccurate, subjective, over-sensitive, and failing to reflect human exposures in the real world.

A powerful extratropical cyclone over the North Pacific Ocean in January 2018, with an eye-like feature and a long cold front extending to the tropics Extratropical cyclones, sometimes called mid-latitude cyclones or wave cyclones, are low-pressure areas which, along with the anticyclones of high- pressure areas, drive the weather over much of the Earth. Extratropical cyclones are capable of producing anything from cloudiness and mild showers to heavy gales, thunderstorms, blizzards, and tornadoes. These types of cyclones are defined as large scale (synoptic) low pressure weather systems that occur in the middle latitudes of the Earth. In contrast with tropical cyclones, extratropical cyclones produce rapid changes in temperature and dew point along broad lines, called weather fronts, about the center of the cyclone.

Early on September 1, the JTWC reported that an area of convectional cloudiness had persisted in an area of low pressure vertical windshear about to the northwest of Manila in the Philippines. The system had a fully exposed low-level circulation center with small pockets of convection confined to the western edge of the cyclone. During the next couple of days the disturbance developed further with deep convection consolidating near the low-level circulation center before being designated as a tropical depression by the JMA and had a Tropical Cyclone Formation Alert issued by the JTWC early on September 3. Later the next day, it made a direct hit on Đà Nẵng, Quảng Nam and Quảng Ngãi, Vietnam and after several hours.

The South Pacific Convergence Zone (SPCZ), a reverse-oriented monsoon trough, is a band of low-level convergence, cloudiness and precipitation extending from the Western Pacific Warm Pool at the maritime continent south-eastwards towards French Polynesia and as far as the Cook Islands (160W, 20S). The SPCZ is a portion of the Intertropical Convergence Zone (ITCZ) which lies in a band extending east–west near the Equator but can be more extratropical in nature, especially east of the International Date Line. It is considered the largest and most important piece of the ITCZ, and has the least dependence upon heating from a nearby landmass during the summer than any other portion of the monsoon trough.E. Linacre and B. Geerts.

A WP-3D Orion weather reconnaissance aircraft in flight The atmosphere is a fluid. As such, the idea of numerical weather prediction is to sample the state of the fluid at a given time and use the equations of fluid dynamics and thermodynamics to estimate the state of the fluid at some time in the future. On land, terrain maps, available at resolutions down to globally, are used to help model atmospheric circulations within regions of rugged topography, in order to better depict features such as downslope winds, mountain waves, and related cloudiness which affects incoming solar radiation. The main inputs from country-based weather services are surface observations from automated weather stations at ground level over land and from weather buoys at sea.

Some jellies, such as redcurrant, or mint, are classic accompaniments to roasted meats such as turkey, game, and lamb. A traditional method for filtering the fruit from the liquid in a jelly is through the use of a muslin or stockinette "jelly bag", suspended by string from an upturned stool over a bowl to allow the straining to occur gently under the action of gravity. Jellies need to be strained very slowly and gently to ensure the clarity of the result, as forced straining by squeezing or pressing can lead to cloudiness in the jelly. Pectin is essential to the formation of jelly because it acts as a gelling agent, meaning when the pectin chains combine, they create a network that results in a gel.

Flight 864 was a regularly scheduled international passenger flight from Rome to Tokyo with stopovers in Cairo, Bombay and Bangkok. With 9 crew members and 44 passengers on board, flight 864 approached Bangkok. At 20:30 GMT (03:30 local time), the crew contacted the approach controller and reported about the distance of 33 nautical miles (61 km) from the airport’s radio beacon. At this time, conditions were reported as calm, with cloudiness from 2/8 to 4/8 at the lower border of 300 meters, air temperature of 25 °C at a dew point of 24°C, visibility of 4000 meters, and an airfield pressure of 1007 mB. Having received the radar vector to the “BK” DPRM, the crew began their approach to runway 21L.

An area of cloudiness and rainshowers developed several hundred miles east-southeast of Bermuda on August 25, likely in association with a low-level disturbance that formed along a cold front. For several days, it moved southwestward, and, while located on the southwestern end of an upper-level trough to the north of Puerto Rico, deep convection throughout the system increased. The system tracked westward, and initially remained disorganized while surface pressures remained high. The system turned to a northwest drift, and began to slowly organize on August 30 while located a few hundred miles northeast of the Bahamas. A broad low- pressure area developed on August 31 though convection remained disorganized as winds of 20 to 25 mph (32 to 40 km/h) were reported in squalls.

As winter transitions toward spring, snowfall drops sharply by March, when lake and land temperatures nearly equalize. In winter, the heavy lake-effect snowfall is augmented by snowfall from sometimes-strong low-pressure systems (mid-latitude cyclones) that often converge on the Great Lakes and areas further east. Overall, Parry Sound experiences a typical humid continental, cool-summer climate type in terms of temperatures - but a highly unusual climate regime in precipitation and cloudiness; the year's driest months are generally from March through July, while its wettest months are from September to January, with autumnal lake effect producing cloudy skies and heavy rainfall from September into November, followed by extremely heavy snowfall in December and January. The highest temperature ever recorded in Parry Sound was on July 6, 1921.

The crew acknowledged the transmission. According to the actual weather forecast at 20:50, at the Funchal airport, near the tower, the wind was blowing at a speed of 06 knots (11 km/h) in the area of the runway - a heading of 200, visibility 5 kilometers, cloudiness 7/8, rain showers, airfield pressure at runway 24: 1006 mbar, at runway 06: 1008 mbar, temperature 18-19 °C. At 9:23:13 the crew reported on the passage of the MAD beacon at a height of 1,700 feet and a heading of 215, while not having visual contact with the ground. Following the course of 200 and descending 980 feet, at 21:26:33 from flight TP-425 they reported that there was no visual observation of the runway and a missed approach.

Tropical Storm Dorian as a tropical wave on July 29 A tropical wave (also called easterly wave, tropical easterly wave, and African easterly wave), in and around the Atlantic Ocean, is a type of atmospheric trough, an elongated area of relatively low air pressure, oriented north to south, which moves from east to west across the tropics, causing areas of cloudiness and thunderstorms. Tropical waves form in the easterly flow along the equatorward side of the subtropical ridge or belt of high air pressure which lies north and south of the Intertropical Convergence Zone (ITCZ). Tropical waves are generally carried westward by the prevailing easterly winds along the tropics and subtropics near the equator. They can lead to the formation of tropical cyclones in the north Atlantic and northeastern Pacific basins.

Groundhog Day (Pennsylvania German: Grund'sau dåk, Grundsaudaag, Grundsow Dawg, Murmeltiertag; Nova Scotia: Daks Day) is a popular American tradition observed in the United States and Canada on February 2. It derives from the Pennsylvania Dutch superstition that if a groundhog emerging from its burrow on this day sees its shadow due to clear weather, it will retreat to its den and winter will persist for six more weeks; but if it does not see its shadow because of cloudiness, spring will arrive early. While the tradition remains popular in modern times, studies have found no consistent correlation between a groundhog seeing its shadow and the subsequent arrival time of spring-like weather. The weather lore was brought from German-speaking areas where the badger (German: dachs) is the forecasting animal.

In summer, cloudiness is reduced (about 25 sunny days in a month) and the duration of sunshine is of 10–12 hours a day. Annual precipitation is low (about ). The sea breeze is stronger in summer. The natural cure factors are the water of the Black Sea, which is chlorided, sulphated, sodic, magnesian, hypotonic (mineralization 15.5g), the sulphurous, chlorided, bicarbonated, sodic, calcic, mesothermal (21-28 °C) mineral waters of the springs in the northern part of the city, in the area of the beach between Saturn and Venus, the sulphurous peat mud, rich in minerals, which is extracted from the peat bog north of the city (expected to last another 250 years) and the marine climate, rich in saline aerosols and solar radiation that have a bracing effect on the organism.

Investigations by the Secretariat of Communications and Transportation prove that the pilot of the helicopter did not lose control of the aircraft. Initial investigations show that the coordinates of where accident occurred coincide with the last record taken by the helicopter's radar. Moreover, government sources mention that the pilot of the helicopter took a different route in an attempt to escape the cloudiness and find a lower and more visible trajectory to their destination, but eventually wrecked in a hill known as Ayaqueme, situated in the municipality of Chalco. Forensic investigations and autopsies show that "...all (the deaths) were (caused by) traumas," since the bodies came very complete, and doctors mention that the cause of death of all occupants of the helicopter was due to a very severe impact.

An elongated surface trough of low pressure began interacting with an upper-level low across the northwestern Caribbean at the start of October, resulting in widespread cloudiness and scattered showers across the region. Despite unusually low surface pressures, strong upper-level winds were initially forecast to prevent significant organization. During the afternoon hours of October 3, satellite imagery and surface observations indicated that a broad area of low pressure had formed over the extreme southwestern Caribbean. The disturbance began to show signs of strengthening almost immediately; satellite images the next morning showed large curved bands of deep convection wrapping into the well-defined center, prompting the National Hurricane Center (NHC) to upgrade it to a tropical depression at 12:00 UTC on October 4, while located about south of San Andres Island.

Beaver has a typical Intermountain Region cool semi-arid climate (Köppen BSk), bordering on a humid continental climate (Dfb), with summers characterized by hot days and chilly nights, and cold winters with moderate snowfall. During the summer, days are hot and usually dry, though on occasions, as in July 1936 – the wettest month on record with – monsoonal weather can bring heavy thunderstorms from the Gulf of California. Owing to the absence of cloudiness caused by the Great Salt Lake, nights are much cooler than in Salt Lake City or Ogden during this season. The hottest recorded temperature in Beaver is , which has occurred twice on June 21, 1913 and July 26, 1931, and 23.3 days will on average top , although the hottest monthly mean minimum is only in July 1968.

Braunschweig was to be largely destroyed, not only as an important centre of the armament industry, but also, and above all, as a living place, thereby making it uninhabitable and useless. The goal, namely the greatest possible destruction, was to be achieved through detailed attack plans and careful execution, and also making careful use of the attributes of the materiel that was to be deployed. The means whereby the goal was to be reached would be the aforesaid firestorm, the production of which was to be no accident; it was scientifically basedJörg Friedrich and developed through painstakingly detailed analysis. On 13 October, the chief meteorologist at RAF High Wycombe advised RAF Bomber Command headquarters of the weather forecast for the weekend of 14–15 October: slight cloudiness, good visibility throughout the night, and moderate winds.

At 00:00 UTC July 5, shortly after the formation of Tropical Storm Edouard, the NHC began to track an area of disorganized cloudiness and showers in relation to a nearly stationary surface trough in the Gulf of Mexico. After meandering over the Gulf, the disturbance moved northeast towards the coast of the Florida Panhandle, and would subsequently move inland by 12:00 UTC July 6. Two days later, the system re- emerged over the coast of Georgia. Once offshore, the system began to organize as deep convection blossomed over the warm waters of the Gulf Stream. Three hours later, the center reformed near the edge of the primary convective mass, prompting the NHC to initiate advisories on Tropical Storm Fay at 21:00 UTC July 9, located just 40 miles east-northeast of Cape Hatteras.

In 1831, the lighthouse was described as having a distinctive occulting characteristic as follows: "This light appears in full force like a star one minute and a half, and is then eclipsed half a minute. It is lighted throughout the night, and is seen at the distance of one or two leagues, according to the state of cloudiness or clearness of the atmosphere". Trinity House soon resolved to replace the lighthouse with "a far more elegant, and much loftier structure, about half a mile northward of the former building, and which, from its greater altitude, as well as from there being no land intervenient to the point of view, must be perceptible at a far greater distance". At the same time, they planned to erect a second light on the foreshore, the two together being designed to function as leading lights.

A tropical wave emerged into the Atlantic from the west coast of Africa at a low-latitude on June 13\. Although the wave was initially accompanied by a large area of showers and thunderstorms, convection diminished later the following day. The National Hurricane Center (NHC) began discussing the system in its Tropical Weather Outlooks (TWO) while the wave was located well south of Cabo Verde on June 14, though any organization was expected to be slow as the system tracked swiftly westward. Deep convection flared sporadically as the wave moved westward under the influence of a mid- level ridge situated to the north during the next few days. On June 16, cloudiness associated with the feature began to show signs of organization. ASCAT data around 12:00 UTC on June 18 indicated that a broad low pressure area developed, but lacked a well-defined circulation.

Each of the named tributaries of the Orinoco River deserves a more detailed study. Also, some problems that are scarcely investigated, such as the different coloration of the waters of these tributaries, as seen in the image, the phenomenon of the lack of cloudiness in the mornings in the mountiest rivers (a phenomenon that is briefly explained in the articles on the Venezuelan Guayana, in the Amazon river and especially in the article on diathermy), the great extension of dunes or dunes in the Apure state, which is located between the Cinaruco, Capanaparo, Arauca and the own rivers Apure, the comparison of the flow between the different tributaries and between the Guaviare and the Orinoco and others, are also issues that deserve separate treatment, something more detailed than the one that is included later in the documentary study of the basin of the great river Columbia-Venezuelan.

When the cloudiness is eliminated from one's heart through self-reflection, something gushes up from inside, which turns into tears and washes off dirt and dust. As one's heart transforms from one that is cloudy to one that is clear, God's light penetrates into the heart and the penetration of God's light also means that one acquires the strengths of other powers as well. Takahashi believed that when people try hard to realize a lifestyle that is based on right judgments made by the heart where there are no biases, their self-righteous heart disappears, and in turn they learn that everyone in the human race are brothers and sisters, and acquire the power of great charity and love. According to Takahashi, charity refers to actions like that of the sun where one provides the energy of heat and light fairly to both good and bad people.

A tropical wave exited the coast of Africa on August 6. It moved westward across the Atlantic Ocean without development, and entered the eastern Pacific Ocean on August 16 after crossing Central America. Cloudiness and convection gradually increased along the wave axis and organized into a distinct area of disturbed weather on August 20 while located a short distance south of Manzanillo, Mexico. It slowly became better organized as it moved northwestward in an area favorable for continued development. With light vertical wind shear and warm water temperatures, the convection concentrated around a developing low-level circulation, and on August 22 it organized enough for the National Hurricane Center to classify it as Tropical Depression Nine-E while it was located about 115 miles (185 km) west of the Mexico mainland or about 220 miles (345 km) southeast of the southern tip of the Baja California Peninsula.

In a 2007 New York Times article, Harold McGee popularized an alternative method for clarifying broths, originating among chefs of the molecular gastronomy movement: gelatin filtration. Gelatin-filtration is a novel method of clarification, relying on some of the properties of a super-saturated solution of gelatin, created by freezing, to remove macroscopic particles that cause cloudiness from a water-based stock. This method is distinct from traditional consommé both in technique and in final product, as gelatin filtration results in a gelatin-free broth, while traditional consommé gives a final product rich in gelatin, with a correspondingly rich mouthfeel. Freezing a water-based solution converts all bulk water into ice crystals, but water associated with solutes—in the case of a soup stock, gelatin, fat, and flavor compounds—remains unfrozen to much lower temperatures; in practice, the freezing temperature of this associated water is well below the reach of conventional freezers.

Extended cloudiness lasting longer than two or three days is rare. Winter typically consists of cool days and cold nights, except following passage of the strongest cold fronts and arctic airmasses when daytime temperatures remain colder than average; overnight temperatures tend to fall below freezing between about 10 pm and 8 am in the city, except during colder airmasses, plus colder spots of the valley and most of the East Mountain areas. December, the coolest month, averages , although extreme low temperatures bottom out in early January; the median or normal coolest temperature of the year is just above , though the average or mean is below . It is typical for daily low temperatures in much of December, January, and February to be below freezing, the long-term average 76 of 90 days falling to or below freezing; four 24 hour days stay below freezing on average, though that often occurs for less hours west of the Rio Grande and in the Heights.

When warm air ahead of an oncoming storm system overrides cool air trapped east of a mountain range, cloudiness and precipitation can occur for prolonged periods of time Cold air damming, or CAD, is a meteorological phenomenon that involves a high-pressure system (anticyclone) accelerating equatorward east of a north-south oriented mountain range due to the formation of a barrier jet behind a cold front associated with the poleward portion of a split upper level trough. Initially, a high-pressure system moves poleward of a north- south mountain range. Once it sloshes over poleward and eastward of the range, the flow around the high banks up against the mountains, forming a barrier jet which funnels cool air down a stretch of land east of the mountains. The higher the mountain chain, the deeper the cold air mass becomes lodged to its east, and the greater impediment it is within the flow pattern and the more resistant it becomes to intrusions of milder air.

On May 1, an area of convectional cloudiness associated with an area of disturbed weather formed southeast of Nha Trang, Vietnam and associated with a remnant of Tropical depression Crising to form a new stronger area of disturbed weather system. JTWC monitored the disturbance as "Fair" for developing due to low vertical wind shear and an upper-level anticyclone to the east of the system. Later on the JMA designated the low pressure as a minor tropical depression reporting the outlook track as southwestward. The JTWC issued a TCFA on the system once the convection increased and became better organized although with an exposed LLC east of its convection. Early morning of May 3, the JMA begun issuing tropical cyclone advisories on the system forecasting it to become a tropical storm later in the afternoon as it tracked eastwards. On May 3, the JTWC designated the disturbance as Tropical Depression 02W, and the JMA named the storm Chan- hom. Later on May 4, Chan-hom strengthened into a severe tropical storm. On May 6, the system moved into the Philippine Area of Responsibility from the west and was named as Emong.