Confidence: Medium-HIgh Tomorrow night: A weak area of low pressure off the coast could lead to some scattered light showers.
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But, remember market timing is often a weak area for investors, hence the common advice, don't try and time the markets.
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Since there are no major faults nearby, Graves said he believes this swarm is likely due to small cracks or a weak area in the Earth's crust.
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Confidence: Medium Tomorrow night: A weak area of high pressure starts to work in behind the departing system, but isn't quite enough to clear out our skies.
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Confidence: Medium-High Light snow or rain may develop Tuesday morning and continue into the afternoon, as a relatively weak area of low pressure tracks just to our south and then off the coast.
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The nor'easter originated in a weak area of surface low pressure that formed over northern Texas by December 25. It moved generally eastward over the next day as it crossed the Deep South.
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When they are initiated, they are given gifts by each of the members of the Tribunal. These gifts can be a strengthening or focusing of existing powers, abilities, additional powers (rare), or reinforcement of a character's weak area.
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Motor Trend, May 1977, p. 41 Braking was described as "excellent", having a decelerating g-force of 0.875.Motor Trend, May 1977, p. 42 The only weak area was performance, the 604 "not coming up the standards of excellence set by ride, handling and stopping ability".
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Southerly vertical wind shear limited its development for much of its life cycle. Turning eastward, it reached its maximum intensity late on the 3rd before shearing apart on December 4. Early on December 5, the system degenerated into a weak area of low pressure.Joint Typhoon Warning Center.
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In 2011, the output was . The company is an important employer in the otherwise economically weak area of the south-central Black Forest. In 2008, the brewery employed 230 people and paid €17 million as dividends to its owner, the state of Baden-Württemberg. It also paid €16.7 million in tax.
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A weak area of low pressure developed south of Java along the monsoon trough on February 2. The system meandered for a few days while becoming better organized. Late on February 5, the Bureau of Meteorology upgraded the low pressure to tropical cyclone intensity. Willy moved southwestward starting on February 6 and continued to intensify.
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Cyclone Bonita originated from a weak area of disturbed weather observed about to the east of Diego Garcia, in the Chagos Archipelago, on December 31, 1995. The system was marked by a distinct low-level circulation and curved banding features,Le Goff, et al., p. 24 and the Joint Typhoon Warning Center (JTWC) promptly began monitoring it.
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Wages, incomes, and personal consumption levels rose at respectable rates despite an overall increase in investment. Agriculture continued to be a weak area but had improved markedly. By 1975 the agricultural sector was almost self-sufficient in animal production, and self- sufficiency in crop production appeared to be an attainable goal. Rural wages rose, and mechanization progressed rapidly.
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Thus, the Gauls selected 60,000 men and appointed Vercassivellaunus, a near relative of Vercingetorix, to lead the attack on that spot. They marched there before dawn and launched the attack at noon. Vercingetorix made a sally and attacked any part of the inner fortification which seemed weak. Caesar sent Labienus to support the defense of the weak area with six cohorts of cavalry.
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A weak area of low pressure developed east of Queensland on January 11. The tropical disturbance moved northeastward over the Coral Sea and gradually became better organized. On January 13 it turned to the south and intensified into a tropical cyclone the next day. In a favorable environment for intensification, Grace strengthened on January 15 and 16, developing a ragged eye as seen on the satellite images.
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On 4 January 2006, a weak area of low pressure was situated in the Arafura Sea. It moved westward, and by 6 January, it was located in the Timor Sea. That same day, both the United States Joint Typhoon Warning Center (JTWC) and the Australian Bureau of Meteorology (BoM) identified the system as a tropical disturbance. On 7 January, the low began to show signs of strengthening.
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This was a particularly weak area of the act. It required the Finance Minister of India to only conduct quarterly reviews of the receipts and expenditures of the Government and place these reports before the Parliament. Deviations to targets set by the Central government for fiscal policy had to be approved by the Parliament. No other measures for failure of compliance have been specified.
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Hippocrates concludes that the degree of damage a given disease can do to a person depends on its nature. The most serious of illnesses are those that affect the strongest part of the body. If the strongest part of the body is affected, then the weak parts are easily affected and may cause death. However, if a disease starts in a weak area of the body, often it is curable.
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On March 25, 2014, a weak area of low pressure accompanied by broad, flaring convection became increasingly organized over Mozambique. Owing to favorable environmental conditions, featuring low wind shear, vorticity became more enhanced and symmetrical. A compact system, the low steadily organized as it emerged over the Mozambique Channel on March 26\. Though continued land interaction initially hindered development, enhanced outflow supported convective development as it straddled the Mozambique–Tanzania border.
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The possibility of tropical cyclogenesis from a tropical disturbance south of Mexico was first mentioned by the National Hurricane Center (NHC) on July 6. A westward-moving tropical wave crossed Central America and entered the Eastern Pacific on July 8. The next day, the wave spawned a weak area of low pressure while south of Guatemala. On July 10, the disturbance quickly organized, with convection, or thunderstorms, more concentrated near the center of the low.
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Tropical Storm Delia originated from a tropical wave that formed over the central Caribbean Sea in late August 1973. Tracking towards the west-northwest, convective activity increased and the overall structure of the system improved. By August 31, a weak area of low pressure formed over the Gulf of Honduras. This system tracked northward and further organized into a tropical depression just off the southeastern coast of the Yucatán Peninsula on September 1.
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Femoral hernias occur just below the inguinal ligament, when abdominal contents pass into the weak area at the posterior wall of the femoral canal. They can be hard to distinguish from the inguinal type (especially when ascending cephalad): however, they generally appear more rounded, and, in contrast to inguinal hernias, there is a strong female preponderance in femoral hernias. The incidence of strangulation in femoral hernias is high. Repair techniques are similar for femoral and inguinal hernia.
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The party won seats in Limerick city, historically a weak area for them in local elections. Its best results were in Cappaghmore-Kilmallock and Limerick City East where they secured 3 seats in each LEA. Fine Gael were disadvantaged by the merger of the 2 local authorities as they held many councillors on the old City Council and several of these Councillors were defeated under the new boundaries. However, the party won 3 seats in Newcastle West.
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On August 13, 2018, the Joint Typhoon Warning Center (JTWC) began monitoring a weak area of low pressure to the south- southeast of the Ryukyu Islands. Disorganized convection accompanied the low, primarily south of the circulation due to strong westerly flow. Environmental conditions consisting of low wind shear, high sea surface temperatures (averaging ), and an anticyclone aloft favored development of the low. At 06:00 UTC the next day, the Japan Meteorological Agency (JMA) classified the system as a tropical depression.
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A weak area of low pressure developed over northwestern Cuba in association with a stationary front on January 6\. The frontal wave intensified as it moved into the central Atlantic, temporarily attaining hurricane-force winds by January 10\. Steered by anomalous high pressure, the disturbance turned southeast and tracked over warmer waters. Its associated fronts dissipated, its wind field became more symmetric, and convection increased near the center, leading to the formation of Subtropical Storm Alex by 18:00 UTC on January 12\.
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In late September 1989, an active monsoon trough over the South China Sea spawned a tropical disturbance near northern Luzon. By September 28, a broad band of convection associated with a weak area of low pressure developed within the trough. Later that day, the Japan Meteorological Agency (JMA) began monitoring the system as a tropical depression. Aided by a well-defined anticyclone, the low quickly organized, prompting the Joint Typhoon Warning Center (JTWC) to issue a Tropical Cyclone Formation Alert.
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Cyclone Carol formed from a weak area of low pressure to the southwest of Timor on December 12. While moving to the southwest, the disturbance developed banding features and was classified as Cyclone Carol. As Carol moved to the west, it intensified and peaked at 195 km/h (120 mph) with a barometric pressure of 940 hPa (27.76 inHg) on December 16. Briefly, both Carol and Dan exhibited a Fujiwhara interaction around December 17 due to their close proximity to each other.
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Hurricane Kyle began as a weak area of low pressure associated with a tropical wave that moved off the west coast of Africa on September 12. The system tracked in a general westward direction with little convective development and tracked over the Leeward Islands on September 18. An upper-level trough situated over the eastern Caribbean Sea interacted with the wave, resulting in an increase in shower and thunderstorm activity. The following day, a larger surface circulation developed as the low moved towards the northwest.
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On September 5, a weak easterly wave moved into the Gulf of Mexico from the Caribbean Sea due to the influence of an upper-level trough. The wave organized and spawned a weak area of circulation which developed into a tropical storm by 0600 UTC on September 7. Moving steadily towards the northeast at roughly , Debbie only marginally strengthened due to the presence of cooler air entrainment. Early on September 8, Debbie made landfall near Fort Walton Beach, Florida as a minimal tropical storm with winds of .
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The first storm of the season developed out of a weak area of low pressure situated about 570 mi (925 km) south-southwest of Acapulco, Mexico. Tracking towards the west, the circulation briefly dissipated on May 30, before redeveloping the following day into Tropical Depression One-E. A ridge of high pressure north of the system steered it towards the west-northwest. By 0600 UTC on June 1, the National Hurricane Center (NHC) upgraded the depression to a tropical storm and gave it the name Adolph.
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Typhoon Faye originated from a westward-moving weak area of disturbed weather located within the Philippine Sea in the middle of August. On August 16, the Joint Typhoon Warning Center (JTWC) started monitoring the disturbance for possible development. Initially, little development was expected due to its close proximity to land and Typhoon Ellis. The disturbance was poorly organized and the atmospheric circulation was exposed from the deep convection despite being located near an anticyclone, which tends to favor tropical cyclogenesis. On August 20, the Japan Meteorological Agency (JMA) started tracking the disturbance.
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The catalyst for the severe weather outbreak came as a positively-tilted shortwave trough progressed across the central High Plains into the Great Plains and eventually through the western Great Lakes region. A weaker disturbance pushed from the Ozarks into the Northeast United States, acting to strengthen southwesterly winds aloft across the risk area. At the surface, a weak area of low pressure initially centered over northeastern Kansas early on April 9 progressed steadily northeast while intensifying, reaching the trisection of Iowa, Wisconsin, and Illinois by late that evening.
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On 22 March 2017, a well-defined but weak area of low pressure developed over the Coral Sea, near the Louisiade Archipelago of Papua New Guinea. Strong wind shear aloft kept the accompanying convection poorly organised and displaced west of the surface circulation. With environmental conditions forecast to improve and favour cyclogenesis, the Australian Bureau of Meteorology's (BOM) Tropical Cyclone Warning Centre in Brisbane classified the system as a tropical low. Throughout the following day, decreasing shear enabled convection to wrap around the low; however, convective activity remained largely transient.
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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.
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Current research shows that tobacco smokers who are exposed to residential radon are twice as likely to develop lung cancer as non-smokers. As well, the risk of developing lung cancer from asbestos exposure is twice as likely for smokers than for non- smokers. New research has found that women who smoke are at significantly increased risk of developing an abdominal aortic aneurysm, a condition in which a weak area of the abdominal aorta expands or bulges, and is the most common form of aortic aneurysm. Smoking leads to an increased risk of bone fractures, especially hip fractures.
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Tropical Cyclone Tasha was first identified on 24 December 2010 by the Joint Typhoon Warning Centre (JTWC) as a weak area of low pressure accompanied by increasing deep convection. At the surface, the structure of the storm's circulation was uncertain as feeder bands provided a clear indication of its centre; however, the lack of westerly winds at the surface refuted this. Situated roughly east-northeast of Cairns, Queensland, favourable environmental conditions, such as low wind shear, would allow for further development of the low. Later on 24 December, the Australian Bureau of Meteorology (BOM) classified the system as a tropical low.
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Seerey made his debut with the Indians on June 9, 1943. Almost immediately after his debut, he earned the nickname of "people's choice" in media due to both his hitting ability and his "willingness to challenge the brick walls of the stadium". He played in 26 games for the Indians on the season, and hit .222 in 72 at-bats. Entering the 1944 Cleveland Indians season, manager Lou Boudreau planned to use Seerey as the starting center fielder, as he had reported to spring training 25 pounds lighter and Boudreau felt that Seerey could improve on a weak area on the team's roster.
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Since late August 1, Noru presented a 95 km (60 mi) diameter large but ragged eye, yet the convective ring surrounding the eye gradually elongated, especially on the northwestern quadrant; meanwhile, microwave imageries even depicted a break from the northwestern portion of the eyewall. Noru was establishing a poleward outflow channel that tapped into a passing mid- latitude trough located to the north on August 2, and a strong near-equatorial ridge was steering the typhoon towards a weak area in the subtropical ridge to the northwest, being the result of that passing mid-latitude trough.
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Westerly winds near the equator – associated with an ongoing El Niño event – assisted in spawning a weak area of low pressure in late November 1991 near the International Date Line. The JTWC began tracking the area on the Significant Tropical Weather Advisory at 06:00 UTC on November 25\. Vertical wind shear prevented strengthening at first, but the disturbance continued to develop. A tropical cyclone formation alert from the Joint Typhoon Warning Center (JTWC) soon followed. The Japan Meteorological Agency (JMA) started tracking the disturbance at 06:00 UTC on November 27, and the JTWC issued their first warning 18 hours later on the depression, naming it 31W.
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A strong tropical wave exited the coast of Africa on August 14, moved westward as a disorganized system, and passed through the Cape Verde islands on August 15. On August 17, a weak area of low pressure developed in the system about 750 miles (1,200 km) west-southwest of the Cape Verde islands. Convection increased over the western portion of the wave axis, and the system began to become better organized on August 18 while located about 1,250 miles (2,000 km) east of the Lesser Antilles. However, convection around the system diminished on August 19, and later that day it began to move through the Lesser Antilles.
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On July 10, a weak area of low pressure formed along a stationary front off the eastern coast of Florida. The disturbance gradually shed this frontal boundary and acquired a well-defined center, leading to the formation of a tropical depression around 00:00 UTC on July 12 to the east of the Florida–Georgia border. It intensified into a tropical storm a little over a day later and further to a Category 1 hurricane early on July 14 as it tracked east-northeast. Based on extrapolation from nearby ship reports, the hurricane is analyzed to have reached peak winds of 90 mph (150 km/h) early on July 15.
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On 5 April 2017, the Australian Bureau of Meteorology began monitoring a developing tropical low located in the northeast Indian Ocean, approximately 710 km (440 mi) east of Christmas Island. The system had been tracking in a generally westwards direction during the previous few days as a weak area of low pressure, but had not been significant enough to warrant the issuance of tropical cyclone warnings. The tropical low tracked south-westwards throughout the day of 5 April, before adopting a course to the south-southwest during the night. On the morning of 6 April, sustained gale-force winds developed on the western side of the system.
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Late on December 3, RSMC Nadi reported that Tropical Disturbance 01F had developed out of a weak area of low pressure to the northeast of Fiji. Over the next few days the disturbance gradually developed before RSMC Nadi reported that it had intensified into a tropical depression late on December 11. During the next day the system intensified further with the JTWC starting to issue warnings declaring it as Tropical Cyclone 04P. Later that day RSMC Nadi reported that Mick had intensified into a category one tropical cyclone and named it as Mick, while it was located about 225 km, (140 mi) to the west of Rotuma.
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At 2 p.m. on the afternoon of July 15, a weak area of low pressure was stationed over eastern South Dakota, adjacent to a warm front that extended southeast through southern Minnesota into eastern Iowa. Ahead (north) of the warm front was an area of hot, dry air: the high temperature for the day at Eau Claire was 93 °F (34 °C), Eau Claire hourly weather data for 7/15/1980 and 93 °F (34 °C) in the Twin Cities. South of the front was very humid, hot air: Cedar Rapids, Iowa had a high temperature of 98 °F (37 °C). Weather radar at 9:39 p.m.
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Severe Tropical Cyclone Chris was first identified by the Australian Bureau of Meteorology (BoM) on 1 February 2002 as a weak area of low pressure over the Timor Sea. Over the following day, the system tracked towards the southwest, eventually reaching a point roughly 340 km (210 mi) northwest of Broome, Western Australia, at which time it was classified as a tropical low. Situated in a region of moderate wind shear and good upper- level divergence, the system gradually intensified. The low initially tracked towards the southeast in response to a monsoonal flow; however, this later shifted towards the south-southwest as system intensified.
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Tropical Cyclone Helen was the first tropical cyclone to bring gale-force winds to Darwin, Australia since 1985. The fourth named storm of the 2007–08 Australian region cyclone season, Helen developed out of a weak area of low pressure in late December over the Top End region of Australia. Generally tracking westward, the system eventually intensified into a tropical cyclone and was given the name Helen on 2 January. By this time, it was situated over the Joseph Bonaparte Gulf and was beginning to retrograde eastward. Late on 4 January, the storm made landfall near Channel Point with winds of 95 km/h (60 mph) though rapidly weakened to a tropical low within 12 hours.
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In manufacturing, the Weld line or Knit line or Meld line is the line where two flow fronts meet when there is the inability of two or more flow fronts to "knit" together, or "weld", during the molding process. These lines usually occur around holes or obstructions and cause locally weak areas in the molded part.KNIT LINES, Texas Plastic Technologies Knit lines are considered molding defects, and occur when the mold or/and material temperatures are set too low: thus the materials will be cold when they meet, so that they do not bond perfectly. This can cause a weak area in the part which can cause breakage when the part is under stress.
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On 4 January, a weak area of low pressure developed within a monsoon trough near Timor. The following day, the Joint Typhoon Warning Center (JTWC) began monitoring the system for possible development into a tropical cyclone. Traveling westward, the system was forecast to intensify as it moved into an area highly favouring tropical cyclogenesis with very warm waters (with sea surface temperatures of ) and low wind shear. Additionally, a nearby anticyclone provided good outflow for the system. Over the following two days, deep convection gradually built around the low and on 7 January, the Tropical Cyclone Warning Centre (TCWC) in Darwin designated the system as Tropical Low 05U, at which time the storm was situated roughly south-southeast of Sumba, Indonesia.
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On April 30, RSMC Nadi started to monitor a weak area of low pressure that had developed to the northwest of the Fijian dependency of Rotuma. Over the next couple of days, the system remained poorly organised under the influence of vertical wind shear, from the northwest as it moved slowly towards the south-southwest. During May 2, subsequently initiated advisories on the system and designated it as Tropical Cyclone 35P, after the vertical wind shear surrounding the system, had relaxed and good outflow had developed aloft. During that day the system started to move towards the south- southeast and rapidly developed before RSMC Nadi reported later that day, that the system had developed into a category 1 tropical cyclone and named it June.
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On September 8, a weak area of low pressure developed along the tail-end of a stationary front across the northern Gulf of Mexico. It quickly organized into a tropical depression by 00:00 UTC the next day, positioned about 170 mi (275 km) southeast of Matamoros, Tamaulipas, and further attained tropical storm intensity twelve hours later. The fledgling system moved north and then northeast, making its first landfall along the Mississippi River Delta with peak winds of 65 mph (100 km/h) around 19:00 UTC on September 10\. The system made its second landfall along Dauphin Island, Alabama, at 23:00 UTC at a slightly reduced intensity. It lost character by 12:00 UTC on September 11 and was last documented about 40 mi (65 km) southwest of Montgomery, Alabama.
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Severe Tropical Storm Chanthu originated out of a weak area of low pressure associated with disorganized deep convective activity located about 480 kilometres (300 mi) east-southeast of Yap on June 5\. Low wind shear and weak diffluence allowed the system to gradually become organized; however, the following day, the Joint Typhoon Warning Center (JTWC) ceased monitoring the system for potential development. By June 7, convection redeveloped around the low and the JTWC resumed monitoring the low; later in the day, the Japan Meteorological Agency JMA, the Regional Specialized Meteorological Center for the western Pacific basin, classified it as a tropical depression. The same day, the depression entered the Area of Responsibility (AoR) of the Philippine Atmospheric, Geophysical and Astronomical Services Administration and was given the local name Gener.
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Typhoon Kirogi originated out of a disorganized area of showers and thunderstorms on June 30, 2000, associated with a weak area of low pressure, situated roughly 650 km (405 mi) east of the Philippine island of Mindanao. The system remained nearly stationary for two days as it became increasingly organized. On July 1, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert as they anticipated the low to develop into a significant tropical cyclone within 24 hours. Around 0600 UTC the following day, the Japan Meteorological Agency (JMA) began monitoring the system as a tropical depression. At the same time, the JTWC also classified the system as Tropical Depression 05W and six hours later, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) began issuing advisories on the same system, classifying it as Tropical Depression Ditang.
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MODIS visible satellite imagery a possible January 2004 tropical cyclone According to a presentation at the Sixth WMO International Workshop on Tropical Cyclones (IWTC-VI), satellite imagery from January 1970 showed that a system with an eyewall had developed behind a cold front and that the system needed further analysis to determine if it was tropical or subtropical. On March 27, 1974, a weak area of low pressure that had originated over the Amazon River started to intensify further. Over the next 48 hours the system quickly developed further and was classified as subtropical, as it developed a banding structure and deep convection near its warm core. On March 29, a north-westerly flow encroached on the systems environment, which caused the system to rapidly move towards 40S and the cold waters that were present to the south of 40°S.
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On June 16, a large, disorganized area of showers and thunderstorms developed in association with a weak area of low pressure well to the southeast of Yap. Gradually, the disturbance became more organized as it moved through an area of moderate wind shear, high sea surface temperatures (estimated at by satellites) and favorable diffluence. Further development of the low prompted the Joint Typhoon Warning Center (JTWC) to issue a Tropical Cyclone Formation Alert on June 20. Around 1800 UTC, the Japan Meteorological Agency (JMA) declared the system as a tropical depression. At this time, the depression was located roughly 405 km (250 mi) northwest of Palau. Tracking steadily northwestward in response to a ridge to the northeast, the depression crossed west of 135°E on June 21 and entered the Philippine Atmospheric, Geophysical and Astronomical Services Administration's (PAGASA) area of responsibility.
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On 4 February 2020, the Met Office issued a yellow weather warning for wind covering all of the United Kingdom across the following weekend due to high confidence in the model forecasts for a potential high-impact storm, although the system involved had not yet formed and no name was issued for it at that time. The next day, Storm Ciara was formally named by the Met Office; in Germany the storm is called Sabine. It formed out of a weak area of low pressure emerging into the Atlantic Ocean from the southeastern United States earlier that day; the precursor system had previously brought heavy snowfall to large tracts of the United States and Eastern Canada, with tornadoes across the southern and mid-Atlantic states. On 6 February, Met Éireann issued a country-wide yellow wind and rain warning for Saturday 8 February through Sunday 9 February, expecting average wind speeds from and gusts up to and rainfall of up to .
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On August 17, the NHC highlighted the potential for tropical cyclogenesis off the western coast of Africa in subsequent days. A weak area of low pressure associated with a tropical wave emerged into the eastern Atlantic three days later, and the disturbance steadily coalesced into a tropical depression by 12:00 UTC on August 22, about 305 mi (490 km) southwest of the southernmost Cabo Verde Islands. The depression organized while heading northwest, intensifying into Tropical Storm Gaston six hours later and attaining hurricane intensity by 12:00 UTC on August 24, in accordance with data from satellites and an NASA Global Hawk unmanned aircraft. After its initial peak in intensity, Gaston's satellite appearance began to degrade as an upper-level low imparted strong southwesterly shear on the cyclone, causing it to weaken back to a tropical storm. Upper-level winds slackened early on August 27, and a timely microwave pass highlighted the presence of a low-level eye well embedded in the storm's central dense overcast, indicating the resumption of Gaston's intensification phase.
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