|Tropical storm (SSHWS/NWS)|
|Formed||August 4, 1993|
|Dissipated||August 11, 1993|
|Highest winds|| 1-minute sustained: 60 mph (95 km/h)|
|Lowest pressure||1002 mbar (hPa); 29.59 inHg|
|Damage||$35.7 million (1993 USD)|
|Areas affected||Windward Islands, Venezuela, Colombia, Costa Rica, Nicaragua|
|Part of the 1993 Atlantic hurricane season|
Tropical Storm Bret was the deadliest natural disaster in Venezuela since the 1967 Caracas earthquake. The third tropical cyclone of 1993 Atlantic hurricane season, Bret formed on August 4 from a westward-moving, African tropical wave. Bret would later peak as a 60 mph (95 km/h) tropical storm as it neared Trinidad. It took an extremely southerly course through the Caribbean, passing over the coasts of Venezuela and Colombia. High terrain in the northern parts of those countries severely disrupted the circulation of the storm, and Bret had weakened to a tropical depression before emerging over the extreme southwestern Caribbean Sea. There, it restrengthened to a tropical storm and made landfall in Nicaragua on August 10, dissipating soon after. Bret's remnants reached the Pacific Ocean, where they ultimately became Hurricane Greg.
Though Bret was only a weak tropical storm, it caused extreme flooding and nearly 200 deaths as it moved through South America, mostly in Venezuela. The first tropical storm to strike the country in 100 years, Bret deluged northern regions with 13.35 in (339 mm) of rainfall. The capital, Caracas, received 4.72 in (120 mm) of rain over just seven hours, resulting in widespread mudslides in the hills around the city that buried houses and carried away cars. There were 173 deaths in the country, and damage was estimated at US$25 million (1993 USD). Volunteers and firefighters helped storm victims cope with the damage, and workers cleared roads to restore transportation.
Outside of Venezuela, Bret first affected Trinidad and Tobago, causing minor flooding and power outages. It passed just south of Curaçao, where the storm damaged the coral reef and the roofs of 17 homes. The storm later brushed northern Colombia, killing one person there, before hitting Central America. In Nicaragua, Bret killed 31 people and left US$3 million in damage, with many coastal towns isolated by floods. There was one death in neighboring Costa Rica and seven in Honduras, all due to flooding. In Central America, damage was compounded by Hurricane Gert moving through the region in early September. Even though the storm caused a very high death toll and major damage, the name Bret was not retired following the season and was used again in the 1999 Atlantic hurricane season.
Tropical Storm Bret originated from a tropical wave—a westward-tracking low-pressure area—that crossed the coast of Africa on August 1, 1993. Throughout its journey across the open Atlantic, the wave retained an impressive cloud structure with an area of deep convection. By August 4, the associated thunderstorm activity consolidated and organized into curved rainbands. The National Hurricane Center (NHC), noting the improving structure and sufficient support from Dvorak intensity estimates, reassessed the wave as a tropical depression at 12:00 UTC that day, the third such system of the annual hurricane season. mi (1,850 km) west-southwest of the Cape Verde Islands.At the time of its classification, it was located along the 10th parallel north over the central Atlantic, about 1,150
With a very resilient high-pressure area to its north, the depression continued moving due west at an unusually low latitude for most of its existence. 5. Initially, the agency expected the storm would attain hurricane status while moving west-northwestward through the Caribbean Sea, although the storm would maintain its westward track. Early on August 6, Bret attained peak winds of 60 mph (95 km/h), fueled by warm waters and increased banding around a central dense overcast. The circulation became exposed late on August 6, but the thunderstorms soon refired over the center. At 07:00 UTC on the next day, Bret struck the island of Trinidad near Galera Point. The storm moved across the northern portion of the island, and later made landfall in northeastern Venezuela near Macuro.The system gradually organized due to low wind shear. After the outflow increased and the circulation became better established, the NHC upgraded the depression to Tropical Storm Bret early on August
After hitting northeastern Venezuela, Bret continued westward through the extreme northern portion of the country. Around 20:00 UTC on August 7, the circulation emerged into the southeastern Caribbean Sea. The circulation weakened and became poorly-defined, although the storm maintained stronger winds to the north. Despite the southerly inflow being disrupted by the mountainous terrain, Bret maintained its circulation while continuing westward, passing just north of Venezuela's capital Caracas. Around 08:00 UTC on August 8, the storm moved back onshore Venezuela near Morrocoy National Park in Falcón state. Later that day, the NHC noted that there was "little if any circulation left to this system", although the agency continued issuing advisory due to the storm's heavy rainfall. However, a circulation emerged into the Gulf of Venezuela, which soon crossed into northeastern Colombia. There, the circulation neared the Pico Cristóbal Colón, the tallest mountain in Colombia with a peak of 18,947 ft (5,775 m). This caused the structure to deteriorate, and on August 9 Bret weakened to tropical depression status with the circulation "practically dissipated", according to the NHC. The Hurricane Hunters had difficulty finding a closed circulation, prompting the NHC to discontinue advisories at 15:00 UTC on August 9.
After moving through the southwestern Caribbean Sea, Bret began to re-develop convection as upper-level conditions became more favorable. 10, surface observations confirmed the presence of a low-level circulation, and the NHC re-issued advisories on the system. The convection continued to organize, prompting the NHC to upgrade Bret again to a tropical storm. The storm strengthened slightly further to a secondary peak of 45 mph (75 km/h). Around 17:00 UTC on August 10, Bret made its final landfall in southern Nicaragua near Bahia Punta Gorda. The circulation moved through the country and turned more to the west-northwest. Operationally, it was believed that Bret survived after crossing Central America and entered the eastern Pacific, as the NHC designated it Tropical Depression Eight-E. Post-storm analysis determined otherwise that Bret dissipated over western Nicaragua, near the Pacific coast on August 11. The remnants continued to the west-northwest, eventually developing into a tropical depression on August 15 off the west coast of Mexico. The system eventually became Hurricane Greg with peak winds of 130 mph (215 km/h), which lasted until August 28.By early on August
In general, Bret was forecast to track farther north than it ultimately did. About 24 hours in advance of the storm, tropical cyclone warnings and watches were issued for the southern Lesser Antilles and Venezuela. The first tropical storm watch was posted late on August 5 from Dominica southward to Trinidad. On the next day, this was upgraded to a tropical storm warning and hurricane watch from Saint Lucia to Trinidad. Tropical storm warnings spread westward through Venezuela along the storm's path, as well as the ABC islands and northern Colombia along the Guajira Peninsula. Later when Bret began reorganizing in the southwestern Caribbean, portions of Nicaragua were under a tropical storm warning only nine hours before the storm struck. The warning covered from Puerto Cabezas, Nicaragua through the entirety of the Costa Rican coastline, as well as San Andrés island offshore.
In Trinidad and Tobago, the government set up shelters and sent home non-essential oil workers. Officials canceled flights and shut the ports as a precaution. 7, weather officials stated that the brunt of the storm had passed and that the storm was weakening; this was before the onslaught of the flooding rains. In neighboring Colombia, officials issued a wind and heavy rain warning in response to the storm. Towns shut off electricity along the coast and canceled flights. Later, about 1,000 people evacuated from eastern Costa Rica, and another 40,000 evacuated from portions of Nicaragua, Flights in the country were canceled due to the storm.Stores and business closed early after locals had stocked up on life supplies. Army troops were deployed in Port of Spain to avert looting. The threat of the storm caused a rise in unleaded oil prices. In Venezuela, boats were ordered to remain at port, while flights were canceled to Isla Margarita and Puerto la Cruz. Rescue workers were mobilized in the capital city of Caracas to prepare in the event of landslides. Ahead of the storm, the head of Sucre state declared a state of emergency, and later Caracas was placed under the same state once the rains began. According to the governor of Venezuela's capital district, local weather media expected the storm to only brush Caracas and surrounding areas; as a result, not all precautions were made. On August
The storm first struck northern Trinidad, producing peak wind gusts of 27 mph (44 km/h) and 4.4 in (111 mm) of rainfall. The winds knocked down trees while the rains caused flooding, resulting in power outages, which affected 35,000 people. The power cable connecting Trinidad with Tobago was cut during the storm, leaving the latter island briefly without power. Ten soldiers were burned while attempting to move a downed wire in Tobago. The storm damaged houses on southern Trinidad and central Tobago. Meanwhile, flood waters devastated local crops, resulting in losses of more than TT$4 million (US$730,000). Infrastructure damage due to inaccessible roads and bridges totaled TT$979,000 (US$179,000). On nearby Grenada, a weather station reported sustained winds of 37 mph (59 km/h), with gusts to 45 mph (85 km/h). A ship known as the Lady Elaine, reported winds of 45 mph (75 km/h), while anchored at Hog Island on the south coast of Grenada.
Passing 70 mi (110 km) to the south, Bret brushed Curaçao with tropical-storm-force winds and light precipitation. A peak wind of 48 mph (77 km/h) was recorded at a local weather station, though strong onshore breeze averaged 30 to 35 mph (45 to 55 km/h). The storm damaged the roofs of 17 homes and caused power outages to the island. Rough surf, with wave heights of 4.9 ft (1.5 m), severely disrupted the coral reef along the south shore, breaking off 25–50% of the reef's branches. In particular, elkhorn (Acropora palmata) and fire coral (Millepora complanata) received extensive damage to their structures. Of the coral reefs, those in shallow waters were worst affected; considerable damage also occurred to pillar coral (Dendrogyra cylindrus), which typically grow at depths of less than 16 ft (5 m) below water. The animals and plants there were affected as well. In addition, nearby Bonaire experienced gusts to gale force during the passage of the storm.
As a minimal tropical storm, Bret moved through northern Colombia.The storm downed a power line onto a house in the city of Maicao, killing one person and injuring another. An oil tanker rode out the storm at Coveñas port, with no effects to it or the nation's oil industry.
Striking eastern Venezuela, Bret produced wind gusts of 44 mph (70 km/h) in Guiria, near where the storm moved ashore. Isla Margarita offshore reported wind gusts of 53 mph (85 km/h), as well as high waves 66 ft (20 m) in height. The capital city Caracas recorded wind gusts of around 31 to 37 mph (50 to 60 km/h); according to news reports, Bret was the first tropical storm to affect Caracas in 100 years. However, the storm's rainfall was more significant. Guanare in western Venezuela reported 13.35 in (339 mm) of rainfall in just 10 hours. Quebrada Seca in Barinas state recorded 11.23 in (285 mm) of rainfall over 24 hours, and in the capital Caracas, 4.72 in (120 mm) of rainfall occurred over just seven hours. The capital ultimately was affected by 10 hours of heavy rainfall. One station in the country recorded 5 in (130 mm) of precipitation in seven hours, setting a nationwide record for the 20th century for the heaviest rainfall over that duration.
The heavy rainfall was the most destructive aspect of Tropical Storm Bret in Venezuela. people perished in Miranda state, and another three deaths were reported in Aragua due to landslides. Residents requested assistance from the local fire company, although disrupted telephone service created an atmosphere of confusion. Strong winds also destroyed the roofs of other houses, and areas were left without power. Portions of the Pan-American Highway and a coastal road were disrupted by landslides, and the state of Barinas was largely isolated due to road blockages. Most roads west of Caracas were likewise blocked.On the offshore Isla Margaria, the rains flooded the primary hospital, and rivers overflowed, although damage was minimal. On the mainland, heavy rainfall caused damaging mudslides and flooding, and entire houses buried in the middle of the night with little notice. Flooded rivers washed away cars and homes in the hills of Caracas, mostly along the flooded La Guarre River. Floodwaters mixed with raw sewage from damaged water lines across the region. Residents returned to damaged homes despite warnings. Damage was worst in Petare, La Vega, and El Valle, all surrounding Caracas on insecure mountainsides. One home was wrecked in Petare, killing four family members. At least 19
Overall, Tropical Storm Bret left over 11,000 people homeless, including 6,000 in Barinas state, and 3,500 in Caracas. Bret left US$25 million in damage and caused 173 deaths in the country, while at least 500 were injured. Most of the deceased were living in poorly built homes around Caracas, where at least 120 people were killed, mainly children. The storm was the deadliest natural disaster in Venezuela since the 1967 Caracas earthquake.
Upon making landfall in Nicaragua, Bret caused severe flooding along the coast that left 25 villages isolated. Rains continued following the storm, preventing areas from being reached, and Tropical Storm Gert brought additional rainfall to the area in early September. Throughout Nicaragua, Bret destroyed 12 bridges and disrupted the drainage systems along the regional road network. Heavy rainfall also caused rivers to overflow, causing heavy damage in adjacent fields that affected rice, cassava, and bananas; about 1,800 hectares (4,500 acres) of rice fields were destroyed. Two villages of the Miskito people were washed away, leaving 500 residents homeless. The storm damaged at least 1,500 houses and destroyed another 850, leaving around 60,000 people temporarily homeless. Bret also destroyed ten churches and ten schools, as well as 25 medical centers. The storm killed nine people offshore when a boat sank in the Corn Islands, and there were 31 deaths overall in the country. The preliminary damage total was around US$3 million, although it did not include crop or infrastructure damage.
The storm brought heavy rainfall and high seas to the east coast of Costa Rica, million in damage. Similarly heavy rain fell in the Mosquitia region of Honduras. Floodwaters reached 7 ft (2.1 m) deep, isolating coastal towns. Overflown rivers and flooding forced about 1,700 people to evacuate by canoe, while some residents rode out the storm on the roofs of their homes. About 16,000 people were left homeless. The storm destroyed over 2,000 hectares (5,540 acres) of various crops, and there were seven deaths in the country. In El Salvador, light winds were also experienced, with moderate rainfall reaching 4.1 in (104 mm) in La Palma, Chalatenango. The storm knocked down trees near the capital San Salvador, temporarily leaving the city without power.as well as gusty winds. One death occurred in the country, as well as US$7.7
Venezuela's then-president Ramón José Velásquez held an emergency meeting to respond to the Bret's heavy damage. workers and volunteers helped in rescue efforts after the mudslides struck Caracas and surrounding areas, assisted by Red Cross volunteers and 800 firefighters. Volunteers provided water and medicine to the affected, while workers emptied residual pools of water to mitigate the spread of disease. Storm victims were temporarily housed at the Fuerte Tiuna army base. Roads were quickly cleared of debris and mud, although many were not reopened initially due to the threat for additional mudslides. Within a week of the storm's passage, telephone service was largely repaired in Caracas and airline travel was restored. After the storm, the United Nations Development Programme (UNDP) provided US$50,000 in emergency spending, and UNICEF sent US$15,000 to buy oral rehydration salts. A Venezuelan radio station held a marathon to collect relief items, such as food or clothing.The president conveyed three days of national mourning due to the storm. About 1,400
After the storm, the Nicaraguan government declared a state of disaster in the North and South Caribbean Coast Autonomous Regions, as well as Tisma in the Masaya Department. 18, the government requested international assistance to cope from the disaster. In response, the United Nations Office for the Coordination of Humanitarian Affairs and the UNDP sent US$70,000 in emergency aid, some of which to be used for fuel to transport medicine and food. The World Food Programme sent 72 tons of food and milk. The countries of Japan and the United States were the first to respond; the former provided $100,000, and the latter sent a Lockheed C-130 Hercules to distribute food. Switzerland later sent US$81,000 as a cash donation, while the European Economic Community sent US$227,000 worth of food and medicine. After Tropical Storm Gert struck in early September, various other countries sent additional money, food, medicine, and other goods.The government sheltered those made homeless in Bluefields along the Atlantic coast. Relief efforts were coordinated by the Comité Nacional de Emergencia to provide aid to the affected storm victims. Officials sent medical crews to the hardest hit areas. This was due to an increased potential for the spread of water-born diseases, the result of ongoing floods and damaged sanitation facilities. Meanwhile, planes flew overhead to determine the extent of damage. On August
The government of Honduras used one helicopter to deliver relief goods to stranded residents on roofs. million in Honduras. Despite Bret's excessive death toll, the name was not retired following the season and was used again in the 1999 season.Persistent rainfall following Bret caused additional flooding and damage, and the damage total between Bret and subsequent Tropical Storm Gert totaled US$60
The 1993 Atlantic hurricane season was a below average Atlantic hurricane season that produced ten tropical cyclones, eight tropical storms, four hurricanes, and one major hurricane. It officially started on June 1 and ended on November 30, dates which conventionally delimit the period during which most tropical cyclones form in the Atlantic Ocean. The first tropical cyclone, Tropical Depression One, developed on May 31, while the final storm, Tropical Depression Ten, dissipated on September 30, well before the average dissipation date of a season's last tropical cyclone; this represented the earliest end to the hurricane season in ten years. The most intense hurricane, Emily, was a Category 3 on the Saffir–Simpson Hurricane Scale that paralleled close to the North Carolina coastline causing minor damage and a few deaths before moving out to sea.
Hurricane Cesar–Douglas was one of the few tropical cyclones to survive the crossover from the Atlantic to east Pacific basin, and was the last to receive two names upon doing so. Hurricane Cesar was the third named storm and second hurricane of the 1996 Atlantic hurricane season. The system formed in the southern Caribbean Sea and affected several countries in South America before crossing Nicaragua and entering the Eastern Pacific where it was renamed Hurricane Douglas, the fourth named storm, third hurricane, and first and strongest major hurricane of the 1996 Pacific hurricane season. The storm killed 113 people in Central and South America and left 29 others missing, mainly due to flooding and mudslides.
Hurricane Joan was a long lived, powerful hurricane that caused death and destruction in over a dozen countries in the Caribbean and Central America. Moving on a due west course for nearly two weeks in October 1988, Hurricane Joan caused widespread flooding and over 200 deaths after moving into Central America. Widespread suffering and economic crises were exacerbated by Joan, primarily across Nicaragua, as heavy rains and high winds impacted those near the hurricane's path.
The 1983 Pacific hurricane season was the longest season ever recorded at that time. It was a very active Pacific hurricane season. The season started on May 15, 1983 in the eastern Pacific, and on June 1, 1983 in the central Pacific, and lasted until November 30, 1983. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. During the 1983 season, there were 21 named storms, which was slightly less than the previous season. Furthermore, twelve of those storms became hurricanes. And eight of the storms reached major hurricane status, or Category 3 or higher on the Saffir–Simpson hurricane wind scale (SSHWS). The decaying 1982–83 El Niño event likely contributed to this level of activity. That same El Niño influenced a very quiet Atlantic hurricane season.
The 1992 North Indian Ocean cyclone season was unofficially the most active year on record for the basin, with 10 tropical storms developing, according to the Joint Typhoon Warning Center (JTWC). There are two main seas in the North Indian Ocean – the Bay of Bengal to the east of the Indian subcontinent – and the Arabian Sea to the west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the JTWC releases unofficial advisories. An average of four to six storms form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD.
Hurricane Calvin was one of three Pacific hurricanes on record to make landfall along the Mexican coast during the month of July. The fourth tropical cyclone, third named storm, and second hurricane of the 1993 Pacific hurricane season, Calvin developed from an area of convection to the south of Mexico on July 4. The following day, the system intensified into a tropical storm, which was named Calvin. Continued strengthening ensued as Calvin curved from its initial westward track northward, and was upgraded to a hurricane on July 6 Calvin eventually turned northwest, and became a Category 2 hurricane on the Saffir–Simpson hurricane wind scale (SSHWS). By July 7, Hurricane Calvin made landfall near Manzanillo at peak strength. Calvin rapidly weakened after landfall, and was a tropical storm when it reemerged into the Pacific Ocean on early on July 8. Despite this, the hurricane did not reintensify, and continued to weaken as it headed rapidly northwestward. As Calvin made a second Mexican landfall near the southern tip of Baja California peninsula late on July 8, it weakened to a tropical depression. Early on July 9, the depression dissipated shortly after entering the Pacific Ocean for a third time.
Typhoon Zeb, known in the Philippines as Typhoon Iliang, was a powerful typhoon that struck the island of Luzon in October 1998. It is tied with Cyclone Ron and Cyclone Susan in terms of minimum pressure, for the most intense tropical cyclone worldwide for 1998. The tenth tropical storm of the season, Zeb formed on October 10 from the monsoon trough near the Caroline Islands. It moved westward initially and quickly intensified. Zeb's inflow briefly spawned another tropical storm, which it ultimately absorbed. Developing an eye, Zeb rapidly intensified into a super typhoon, officially reaching maximum sustained winds of 205 km/h (125 mph); one warning agency estimated winds as high as 285 km/h (180 mph). After reaching peak intensity, the typhoon struck northern Luzon and quickly weakened over land. Turning to the north, Zeb brushed the east coast of Taiwan at a reduced intensity, and after accelerating to the northeast it moved through Japan. It became extratropical on October 18 and moved eastward over open waters.
The 1995 North Indian Ocean cyclone season was below-average and was primarily confined to the autumn months, with the exception of three short-lived deep depressions in May. There were eight depressions in the basin, which is Indian Ocean north of the equator. The basin is subdivided between the Bay of Bengal and the Arabian Sea on the east and west coasts of India, respectively. Storms were tracked by the India Meteorological Department (IMD), which is the basin's Regional Specialized Meteorological Center, as well as the American-based Joint Typhoon Warning Center (JTWC) on an unofficial basis.
The 1996 North Indian Ocean cyclone season featured several deadly tropical cyclones, with over 2,000 people killed during the year. The India Meteorological Department (IMD) – the Regional Specialized Meteorological Center for the northern Indian Ocean as recognized by the World Meteorological Organization – issued warnings for nine tropical cyclones in the region. Storms were also tracked on an unofficial basis by the American-based Joint Typhoon Warning Center, which observed one additional storm. The basin is split between the Bay of Bengal off the east coast of India and the Arabian Sea off the west coast. During the year, the activity was affected by the monsoon season, with most storms forming in June or after October.
Severe Tropical Cyclone Olivia was a powerful cyclone, the 13th named storm of the 1995–96 Australian region cyclone season, which formed on 3 April 1996 to the north of Australia's Northern Territory. The storm moved generally to the southwest, gradually intensifying off Western Australia. On 8 April, Olivia intensified into a severe tropical cyclone and subsequently turned more to the south, steered by a passing trough. On the morning of 10 April, passing over Barrow Island off the Western Australian northwest coast, Olivia produced the strongest non-tornadic winds ever recorded, with peak gusts of 409 kilometres per hour (254 mph). On the same day the cyclone made landfall on the Pilbara coast, about 75 kilometres (47 mi) north-northwest of Pannawonica. The storm quickly weakened over land, dissipating over the Great Australian Bight on 12 April.
Tropical Storm Alma, the first named storm to develop in the 1974 Atlantic hurricane season, was a short lived tropical cyclone that made a rare Venezuelan landfall. The storm formed from the Intertropical Convergence Zone (ITCZ) on August 12 well to the east of the Windward Islands, but advisories were not issued until the next day when Alma was at peak intensity. Alma entered the southeastern Caribbean Sea at an unusually brisk westward pace of between 20 mph (32 km/h) to 25 mph (40 km/h), prompting numerous watches and gale warnings throughout the nations in this region. After crossing Trinidad, Alma became one of only four tropical storms to traverse the Paria Peninsula of northeastern Venezuela. The storm dissipated on August 15 over the high terrain of Venezuela.
Typhoon Alex, known in the Philippines as Typhoon Etang, affected the Taiwan, China, and South Korea during July 1987. Typhoon Alex developed from the monsoon trough that spawned a tropical disturbance late on July 21 southwest of Guam which organized into a tropical depression shortly thereafter. The system steadily became better organized, and the next day, a tropical depression had developed. Satellite intensity estimates gradually increased, and on July 23, the depression intensified into Tropical Storm Alex. After initially tracking west-northwest, Tropical Storm Alex started tracking northwest. An eye developed on July 24, and on the next day, Alex was classified as a typhoon, when Alex attained its peak intensity of 120 km/h (75 mph) and a minimum barometric pressure of 970 mbar (29 inHg). Alex weakened while tracking more northward, though interaction with Taiwan resulted in a more westward track starting on July 27. The storm struck near Shanghai as a tropical storm, and weakened over land, although it remained identifiable through August 2.
The 1933 Trinidad hurricane was the easternmost tropical storm to form in the Main Development Region (MDR) so early in the calendar year on record and was one of three North Atlantic tropical cyclones on record to produce hurricane-force winds in Venezuela. The second tropical storm and first hurricane of the extremely active 1933 Atlantic hurricane season, the system formed on June 24 to the east of the Lesser Antilles. It moved westward and attained hurricane status before striking Trinidad on June 27. The storm caused heavy damage on the island, estimated at around $3 million. The strong winds downed trees and destroyed hundreds of houses, leaving about 1,000 people homeless. Later, the hurricane crossed the northeastern portion of Venezuela, where power outages and damaged houses were reported.
Typhoon Sinlaku was a damaging typhoon that affected Okinawa, Taiwan, and eastern China in September 2002. The 16th named storm of the 2002 Pacific typhoon season, Sinlaku formed on August 27 northeast of the Northern Marianas Islands. After initially moving to the north, it began a generally westward motion that it maintained for the rest of its duration. Sinlaku strengthened into a typhoon and attained its peak winds on August 31. Over the next few days, it fluctuated slightly in intensity while moving over or near the Ryukyu Islands. On September 4, the typhoon's eye crossed over Okinawa. It dropped heavy rainfall and produced strong winds that left over 100,000 people without power. Damage on the island was estimated at $14.3 million.
Typhoon Rammasun, known in the Philippines as Typhoon Florita, was the first of four typhoons to contribute to heavy rainfall and deadly flooding in the Philippines in July 2002. The fifth tropical cyclone of the 2002 Pacific typhoon season, Rammasun developed around the same time as Typhoon Chataan, only further to the west. The storm tracked northwestward toward Taiwan, and on July 2 it attained its peak intensity with winds of 160 km/h (100 mph). Rammasun turned northward, passing east of Taiwan and China. In Taiwan, the outer rainbands dropped rainfall that alleviated drought conditions. In China, the rainfall occurred after previously wet conditions, resulting in additional flooding, although damage was less than expected; there was about $85 million in crop and fishery damage in one province.
Severe Tropical Cyclone Bobby set numerous monthly rainfall records in parts of the Goldfields-Esperance regions of Western Australia, dropping up to 400 mm (16 in) of rain in February 1995. The fourth named storm of the 1994–95 Australian region cyclone season, Bobby developed as a tropical low embedded within a monsoon trough situated north of the Northern Territory coastline on 19 February. The storm gradually drifted southwestward and later southward under low wind shear, strengthening enough to be assigned the name Bobby by the Australian Bureau of Meteorology (BoM). The storm rapidly deepened as it approached the coast of Western Australia, and attained its peak intensity of 925 mbar at 0900 UTC on 24 February with 10-minute maximum sustained winds of 195 km/h (120 mph). After making landfall as a somewhat weaker cyclone near Onslow, the remnants of Bobby drifted southeastward, gradually weakening, before dissipating over the southern reaches of Western Australia.
The October 1996 India cyclone had an unusual and protracted path that spanned much of the northern Indian Ocean. It originated in a weather disturbance that formed on October 14 in the southern Bay of Bengal, off India's east coast. Moving westward, it struck Andhra Pradesh on October 17 as a well-defined low-pressure area. It crossed southern India and reorganized in the Arabian Sea off the western coast of India. The system developed into a depression on October 22 and quickly intensified while moving northward. By October 24, the cyclone approached hurricane intensity as it developed an eye, reaching peak winds of at least 110 km/h (70 mph). On October 25, the storm abruptly stalled and weakened off Gujarat, and progressed southwestward as a minimal storm. It was no longer classifiable as a tropical cyclone by October 28, although its remnants persisted until November 2 when they dissipated east of Somalia.
Tropical Storm Bret was the earliest named storm to develop in the Main Development Region of the Atlantic basin on record. Bret formed from a low-latitude tropical wave that had moved off the coast of Africa on June 12. The disturbance moved swiftly across the Atlantic for several days, steadily organizing despite its low latitude. On June 18, the organization increased enough for the National Hurricane Center (NHC) to begin issuing warnings disturbance while it was located southeast of the Windward Islands. The system continued to organize, and by the next day, it had developed into a tropical storm, the second of the 2017 Atlantic hurricane season. Bret continued moving swiftly to the west and struck Trinidad and Tobago early on June 20, before entering the Caribbean Sea, dissipating shortly afterwards.
Tropical Storm Karen was a weak tropical storm that impacted the Lesser Antilles, Virgin Islands, and Puerto Rico in September 2019. The twelfth tropical cyclone and eleventh named storm of the 2019 Atlantic hurricane season, it originated from a tropical wave which entered the tropical Atlantic on September 14. The wave quickly organized as it neared the Windward Islands on September 20, becoming a tropical depression just two days later. The depression strengthened into Tropical Storm Karen later that day, as it moved across the southern Windward Islands. By 18:00 UTC that day, Karen had reached its first peak intensity with 1-minute sustained winds of 45 mph (72 km/h) and a minimum pressure of 1003 millibars. Karen weakened back to a tropical depression at 06:00 UTC on September 23. However, just 12 hours later, Karen re-intensified into a tropical storm. It then entered the central Atlantic, early the next day. Karen began to degrade on September 27, when it weakened into a tropical depression, due to strong wind shear. The system subsequently degenerated into a surface trough later that day.