Instruct: Given a question, retrieve passages that can help answer the question.
Query: What was the first storm to develop in the 1999–2000 South-West Indian Ocean tropical cyclone season?
The 1999–2000 South-West Indian Ocean tropical cyclone season was the first on record in which two storms – Leon–Eline and Hudah – struck Mozambique at tropical cyclone intensity, or with maximum sustained winds of at least 120 km/h (75 mph). The most notable storm of the season was Eline, which was the longest-lasting storm on record in the basin. It lasted for 29 days while traversing the southern Indian Ocean, making the strongest landfall in decades along eastern Madagascar in late February. The storm was the first in a series of three storms that struck the country in early 2000, along with Gloria in March and Hudah in April. Collectively, the three storms killed at least 316 people. The season started on November 1, 1999, and ended for most of the basin on April 30, 2000; for Mauritius and the Seychelles, the season continued until May 15. These dates conventionally delimit the period of each year when most tropical cyclones form in the basin;
The 2013–14 South-West Indian Ocean cyclone season was an above average event in tropical cyclone formation. The season officially began on July 1, 2013, though the first tropical system designated by Météo-France was a short-lived tropical disturbance that developed on July 8. However, the first named storm was Cyclone Amara in December. Bruce was the first very intense tropical cyclone since Edzani in 2010, which originated from the Australian region. The strongest system of the cyclone season was Hellen, also one of the most intense tropical cyclones over the Mozambique Channel. The season officially ended on June 30, 2014
The 1990 Atlantic hurricane season featured the most named storms of any hurricane season at the time. During the season, 14 tropical cyclones in the Atlantic Ocean became named storms. Although Tropical Depression One formed on May 24, the season officially began on June 1; it ended on November 30, dates that conventionally delimit the period of each year when most tropical cyclones develop in the Atlantic basin. The season's final storm, Hurricane Nana, dissipated on October 21.
1899 San Ciriaco hurricane, also known as the 1899 Puerto Rico Hurricane or The Great Bahamas Hurricane of 1899, was the longest-lived Atlantic hurricane on record, and the second-longest-lived tropical cyclone globally on record (in terms of tropical duration) after Hurricane John in the Pacific. The third tropical cyclone and first major hurricane of the season, this storm was first observed southwest of Cape Verde on August 3. It slowly strengthened while heading steadily west-northwestward across the Atlantic Ocean and reached hurricane status by late on August 5. During the following 48 hours, it deepened further, reaching Category 4 on the modern day Saffir–Simpson hurricane wind scale (SSHWS) before crossing the Leeward Islands on August 7. Later that day, the storm peaked winds of 150 mph (240 km/h). The storm weakened slightly before making landfall in Guayama, Puerto Rico with winds of 140 mph (220 km/h) on August 8. Several hours later, it emerged into the southwestern Atlantic as a Category 3 hurricane. The system paralleled the north coast of Dominican Republic and then crossed the Bahamas, striking several islands. Thereafter, it began heading northward on August 14, while centered east of Florida. Early on the following day, the storm re-curved northeastward and appeared to be heading out to sea. However, by August 17, it turned back to the northwest and made landfall near Hatteras, North Carolina early on the following day. No stronger hurricane has made landfall on the Outer Banks since the San Ciriaco hurricane.
Tropical cyclogenesis first occurred in the month of June, with two tropical depressions developing in the Atlantic. However, no tropical cyclones developed in the month of July, the first phenomenon since 1993. In August, five tropical cyclones developed, most notably, Hurricane Alberto. September was more active, with seven named storms forming; that month featured Hurricane Keith, the strongest system of the 2000 Atlantic hurricane season. With seven named storms forming in September, this made it the most active September on record at the time. This record was surpassed two years later when eight storms formed in September. In addition, a quick succession of eight storms occurred in September, and lasted into early October. Six tropical cyclones existed in October and one additional subtropical storm developed in the last week of the month. Following an active October, no tropical cyclogenesis occurred in November, which is the final month of the season.
The 2000 Pacific hurricane season was an above-average Pacific hurricane season, although most of the storms were weak and short-lived. There were few notable storms this year. Tropical Storms Miriam, Norman, and Rosa all made landfall in Mexico with minimal impact. Hurricane Daniel briefly threatened the U.S. state of Hawaii while weakening. Hurricane Carlotta was the strongest storm of the year and the second-strongest June hurricane in recorded history. Carlotta killed 18 people when it sank a freighter. Overall, the season was significantly more active than the previous season, with 19 tropical storms. In addition, six hurricanes developed. Furthermore, there were total of two major hurricanes, Category 3 or greater on the Saffir–Simpson hurricane wind scale.
In August, a tropical depression developed in the south-west Indian Ocean for the first time 27 years, and a month later, a rare September tropical disturbance formed. The first named storm, Antoinette, was the first of several to originate in the neighboring Australian basin, or east of 90° E; the subsequent two named storms also formed in the Australian region. In early December, Cyclone Daniella likely developed out of the remnants of previous Tropical Storm Chantelle. After reaching peak 10–minute winds of 185 km/h (115 mph), Daniella weakened and passed just southwest of Mauritius; there, the storm left heavy crop damage and indirectly caused three deaths. In early January, Tropical Storm Fabriola was the first in a succession of three storms to move over Madagascar. The next – Cyclone Gretelle – killed 152 people when it struck southeastern Madagascar. Between January and February, Cyclone Pancho-Helinda lasted about 20 days between both the Australian and south-west Indian basins. Also in February, Tropical Storm Josie killed 36 people in western Madagascar after causing severe flooding. The final named storm was Tropical Storm Lisette, which dissipated on March 3 after striking Mozambique, killing three people. Despite the early end to the named storms, there were two additional disturbances, one of which became the first July tropical depression in 25 years.
The 1990 Pacific hurricane season saw a then-record 16 hurricanes form. Throughout the year, 21 tropical cyclones became named storms in the eastern Pacific Ocean. Hurricane Alma formed on May 12, 1990, three days before the season's official start on May 15. The Central Pacific hurricane season began on June 1, covering tropical cyclone formation in the region between 140°W and International Dateline. Hurricane Trudy was the last storm to dissipate, doing so on November 1, nearly a month before the Pacific hurricane season officially ended on November 30.
The same monsoon trough that spawned Connie also produced an area of convection southeast of Diego Garcia on January 28. The circulation slowly organized, and the MFR classified it as a tropical disturbance on January 30. A nearby trough steered the system southeastward initially and later to the southwest. On January 31, the system became a tropical depression, and later Moderate Tropical Storm Damienne the next day, reaching peak winds of 65 km/h (40 mph). Also on February 1, the JTWC initiated warnings on Tropical Cyclone 10S, which estimated 1‑minute winds of 95 km/h (60 mph). Increased wind shear removed the convection on February 2, causing marked weakening, and prompting the JTWC to discontinue advisories that day. This was despite forecasts of strengthening to near tropical cyclone status. As a weak tropical disturbance, Damienne turned to a rapid westward motion, passing north of Rodrigues and Tromelin. The circulation dissipated on February 7 off the northeast coast of Madagascar.
On February 1, a low-pressure area formed within the monsoon trough to the south of Indonesia, which would eventually become Tropical Cyclone Leon in the Australian basin, as well as Tropical Cyclone 11S according to JTWC. The storm tracked westward across much of the Indian Ocean, fluctuating in strength due to changes in the atmosphere. After crossing 90° E, the MFR began tracking the system as Tropical Storm Eline on February 8. The storm continued westward across the Indian Ocean and intensified greatly as it approached the east coast of Madagascar. Late on February 17, Eline made landfall near Mahanoro with 10‑minute winds of 165 km/h (105 mph), making it the strongest storm to hit the country in several decades. The storm rapidly weakened over land, but restrengthened in the Mozambique Channel to reach peak 10‑minute winds of 185 km/h (115 mph). On February 22, Eline made landfall about 80 km (50 mi) south of Beira, Mozambique near peak intensity and quickly weakened over land. The well-defined circulation moved across southern African, finally dissipating over eastern Namibia on February 29. Throughout its duration, Leon–Eline lasted 29 days, a record longevity for a storm in the south-west Indian Ocean. The track was over 11,000 km (6,800 mi), or about 25% of the Earth's circumference.
Activity in the season began slowly, with the first tropical cyclone not forming until July 27. It did not become Tropical Storm Alex until July 29, which was an abnormally late first named storm for an Atlantic hurricane season. After being dormant for about two weeks, Hurricane Bonnie developed on August 19. Thereafter, tropical cyclogenesis became more frequent, with an additional three storms by the end of August. September was the most active month, coinciding with the climatological peak of the season. Six tropical cyclones formed in that month, four of which reached hurricane intensity. Four hurricanes were active on September 26, with Georges over the Straits of Florida, Ivan in the North Atlantic, Jeanne was located near Cape Verde, and Karl was situated over the Central Atlantic. This was the first such occurrence since August 22 in 1893. However, three hurricanes also co-existed in the Atlantic on September 11 in 1961, with a possible fourth. Following a busy September, activity began slowing, starting in October, when only two tropical cyclones developed. However, both storms became a hurricane, with the second cyclone, Hurricane Mitch, become the most intense, deadliest, and costliest storm of the 1998 Atlantic hurricane season.
Despite the destructive nature of the season, it began later than usual. Cyclone Astride originated toward the end of December, bringing rainfall and gusty winds to northern Madagascar while in the region. In January, cyclones Babiola and Connie both formed east of Madagascar and took southerly tracks. Connie passed near Réunion island, producing of rainfall in the mountainous peaks and killing two people. Eline, the longest lasting storm of the season, struck Mozambique while the country was experiencing its worst flooding in 50 years, collectively causing around 700 deaths and about $500 million in damage. The storm also killed 12 people in Zimbabwe and 21 in South Africa. Just two weeks after Eline struck Madagascar, Tropical Storm Gloria affected the same general region, bringing additional deaths and damage. Cyclone Hudah in April was the strongest storm of the season, reaching peak 10‑minute winds of 220 km/h (140 mph). It caused three deaths in Mozambique, although its effects were worse in Madagascar, where there were 111 deaths. The final storm of the season was Tropical Storm Innocente, which dissipated on April 24. In addition to the named storms, there were four unnamed tropical disturbances or storms, as well as one subtropical cyclone that formed in the southern Mozambique Channel.
The 1990 Pacific hurricane season was a very active season which observed 21 named storms within the basin. The season also produced the fourth highest ACE index value on record. The season was officially started on May 15 in the eastern Pacific, and on June 1 in the central Pacific, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean. However, these bounds were slightly exceeded when Hurricane Alma formed on May 12.
At the end of September 1979, three circulations developed within the monsoon trough that extended from the Philippines to the Marshall Islands. The westernmost disturbance developed into a tropical depression on October 1, to the west of Luzon, which would later become Typhoon Sarah on October 7. On October 3, the disturbance southwest of Guam developed into Tropical Storm Roger, and later on the same day, a third tropical disturbance that would later become Typhoon Tip formed south of Pohnpei. Strong flow from across the equator was drawn into Roger's wind circulation, initially preventing significant development of the precursor disturbance to Tip. Despite the unfavorable air pattern, the tropical disturbance gradually organized as it moved westward. Due to the large-scale circulation pattern of Tropical Storm Roger, Tip's precursor moved erratically and slowly executed a cyclonic loop to the southeast of Chuuk. A reconnaissance aircraft flight into the system late on October 4 confirmed the existence of a closed low-level circulation, and early on October 5, the Joint Typhoon Warning Center (JTWC) issued its first warning on Tropical Depression Twenty-Three-W.
While executing a loop near Chuuk, the tropical depression intensified into Tropical Storm Tip, though the storm failed to organize significantly due to the influence of Tropical Storm Roger. Reconnaissance aircraft provided the track of the surface circulation, since satellite imagery estimated the center was about from its true position. After drifting erratically for several days, Tip began a steady northwest motion on October 8. By that time, Tropical Storm Roger had become an extratropical cyclone, resulting in the southerly flow to be entrained into Tip. An area of a tropical upper tropospheric trough moved north of Guam at the time, providing an excellent outflow channel north of Tip. Initially, Tip was predicted to continue northwestward and make landfall on Guam, though instead, it turned to the west early on October 9, passing about south of Guam. Later that day, Tip intensified to attain typhoon status.
The New Year's Day Storm () was a powerful European windstorm that affected much of northern Scotland and western Norway on 1 January 1992. DNMI estimated the strongest sustained winds (10 min. average) and the strongest gusts to have reached 90 knots (46 m/s) and 62 m/s, respectively. Unofficial records of gusts in excess of 130 knots (67 m/s) were recorded in Shetland, while Statfjord-B in the North Sea recorded wind gusts in excess of 145 knots (75 m/s). There were very few fatalities, mainly due to the rather low population of the islands, and the fact that the islanders are used to powerful wind, and because it struck in the morning on a public holiday when people were indoors. In Norway there were one fatality, in Frei, Møre og Romsdal county. There were also two fatalities on Unst in the Shetland Isles.
The strongest post monsoon storm ever recorded in Pakistan's recorded history took place on 3 September on a very low pressure system which started to affect parts of Jammu and Kashmir and northeast Pakistani districts of Sialkot, Lahore, Narowal city|Gujrat]], Mandi Bahauddin, Gujranwala, Hafizabad, Sheikhupura. By fourth, the rains became more widespread as the northern Punjab, Pakistan, Azad Kashmir and Khyber Pakhtunkhwa including the twin cities of Rawalpindi/Islamabad, Mangla, Rawalakot, Kotli and Jhelum. The heaviest amounts of rainfall however were recorded on 4 and 5 September as several weather stations broke their 24-hour, 48-hour and total monthly rainfall records for the month of September.
Hurricane Carlotta was the most powerful hurricane of the 2000 Pacific hurricane season. The third tropical cyclone of the season, Carlotta developed from a tropical wave on June 18 about 270 miles (470 km) southeast off the coast of Mexico. With favorable conditions for development, it strengthened steadily at first, followed by a period of rapid deepening to peak winds of 155 mph (250 km/h) on June 22. Cooler waters caused Carlotta to gradually weaken, and on June 25 it degenerated into a remnant area of low pressure while located about 260 miles (420 km) west-southwest of Cabo San Lucas.
The 1969 Atlantic hurricane season officially began on June 1. Of the twenty-four tropical cyclones that developed in the North Atlantic Ocean in 1969, eighteen of them intensified into tropical storms; this was above the 1950–2000 average of 9.6 named storms. In terms of tropical storms, it was the busiest season since 1933. Twelve of the eighteen named storms reached hurricane status, a record that stood until there were fifteen named storms in 2005. Five of the hurricanes deepened into major hurricanes, which are Category 3 or higher on the Saffir–Simpson hurricane wind scale. Between 1950 and 2000, there was an average of 2.3 major hurricanes per season. Throughout the season, the U.S. Weather Bureau issued more advisories than in any previous season. Additionally, reconnaissance aircraft were utilized for more flight hours than in any year in the Atlantic basin until that point. The season officially ended on November 30.
The hurricane season officially began on June 1, though the first tropical cyclone developed on May 21. A total of 21 tropical and subtropical cyclones formed, but just 10 of them intensified into nameable storm systems. This was about average compared to the 1950–2000 average of 9.6 named storms. Six of these reached hurricane status, around the 1950–2000 average of 5.9. Furthermore, three storms reached major hurricane status; close to the 1950–2000 average of 2.3. Collectively, the cyclones of this season caused at least 84 deaths and about $101.63 million in damage. The Atlantic hurricane season officially ended on November 30, with the final cyclone becoming extratropical on October 28.
During the 1990s, the Atlantic Ocean moved into its active era, which led to more tropical cyclones forming during the hurricane seasons. The decade featured Hurricane Andrew which at the time was the costliest hurricane on record, and also Hurricane Mitch which is considered to be the deadliest tropical cyclone to have its name retired killing over 11,000 people in Central America. A total of 15 names were retired in this decade, with seven of those during the 1995 and 1996 seasons. Cumulatively, the 15 systems caused over in damage while over 12145 people lost their lives. There were no names retired for the 1993, 1994 and 1997 seasons.
The 1899 San Ciriaco hurricane1899 San Ciriaco hurricane hit Puerto Rico, whose economy relied on coffee. The crop had already been facing problems with a decrease in prices and competing countries, but the hurricane wiped out any chance of rebounding from the losses of the previous years. The winds stripped the berries from the trees and the coffee exports of 1899 were only 10 percent of the average export. The losses amounted to 12 million dollars in revenue from 1899 to 1901. This left a dismal outlook on the future for farmers. Sugar was also affected by the storm, although the results were not as drastic. Only a third of the sugar crop could be harvested in 1899, but the soil was reinvigorated. The storm only affected the older haciendas, which would have been retired soon regardless of the hurricane. This allowed for newer technologies to be introduced to the sugar system and U.S. involvement increased. Overall, San Ciriaco helped and hurt the agriculture of Puerto Rico.
Since 1850, only seven tropical cyclones have brought gale-force winds to the Southwestern United States. They are: The 1858 San Diego hurricane that was reconstructed as just missing landfall in 1858, the 1939 Long Beach tropical storm that made landfall near San Pedro in 1939, the remnants of Tropical Storm Jennifer-Katherine in 1963, the remnants of Hurricane Emily in 1965, the remnants of Hurricane Joanne in 1972, the remnants of Hurricane Kathleen in 1976, and Hurricane Nora in 1997, after it was downgraded to a tropical storm.
The season began later than usual, the third consecutive one to do so. There were no indications of tropical cyclogenesis before the middle of December, putting the season among the latest 20% since 1967 in terms of seasons' first storms. On December 26, the MFR utilized the QuikSCAT satellite for the first time in the basin to assess a storm's intensity. During the season, 14 tropical disturbances formed, which is near average, and they tended to last longer than normal. Eleven of these disturbances became tropical depressions, of which nine attained gale force winds and were named. In addition, four storms reached tropical cyclone intensity, or 10‑minute sustained winds of 120 km/h (75 mph). The 9 named storms and 4 tropical cyclones is also the basin average for each category in a given year. There were 61 days in which a storm was active, greater than the median of 48 and more than double than the previous season. In general, storms formed south of 10° S, with the exception of the first storm Astride, and most storms generally tracked east to west due to a strong ridge east of Madagascar.
The 2000–01 South-West Indian Ocean cyclone season was a fairly quiet season with only five named storms, although there was an additional unnamed tropical storm and two subtropical cyclones with gale-force winds. It started early, with a tropical disturbance forming on August 1 – the first day of the cyclone year. However, the first named storm, Ando, was not named until January 2, which at the time was the 4th latest on record. Ando would become the most intense cyclone of the year, reaching peak winds of 195 km/h (120 mph) according to the Météo-France office (MFR) on Réunion, the official Regional Specialized Meteorological Center for the basin. The agency tracked storms south of the Equator and west of 90°E to the east coast of Africa.
As a developing disturbance, Gloria produced winds approaching gale-force on St. Brandon. Similar conditions were reported on Tromelin. When Gloria struck Madagascar, it produced sustained winds of 72 km/h (45 mph) at Antalaha, about 70 km (45 mi) south of Sambava. The storm brought heavy rainfall, with Mananjary reporting a two‑day total of . The rains from Gloria occurred less than two weeks after Cyclone Leon–Eline struck the country, bringing additional flooding, landslides, and damage. In Sambava, near where Gloria moved ashore, the storm killed 18 people, destroyed hundreds of homes, and damaged a road connecting the area to the capital of Madagascar, Antananarivo. Farther inland, the cyclone killed 40 people at Andapa. Overall, Gloria killed at least 66 people, although the exact toll was initially unknown due to disrupted communications. Before Gloria emerged into the Mozambique Channel, various news outlets noted the potential for the storm to affect storm-ravaged Mozambique. However, minimal rainfall accompanied Gloria's final landfall. The rains were enough to delay flights for a day, which were transporting relief aid following Eline's devastating landfall in Mozambique.
A tropical low formed in the Australian basin on March 24, moving westward due to a strong subtropical ridge to the south. Despite having intensified enough, the Bureau of Meteorology did not name the system, and on March 25 the system crossed into the South-West Indian Ocean, whereupon it was named Hudah. An eye formed, and the storm intensified into a tropical cyclone on March 27 well to the southeast of Diego Garcia. The structure fluctuated due to dry air, although Hudah was able to intensify steadily on March 31 after conditions became more favorable. The next day, the MFR upgraded it to a very intense tropical cyclone, estimating peak 10‑minute winds of 225 km/h (140 mph). By contrast, the JTWC estimated 1‑minute winds of 235 km/h (145 mph). Cyclone Hudah maintained peak winds until making landfall just southeast of Antalaha, Madagascar on April 2. It weakened greatly over land, but like Eline it re-intensified over the Mozambique Channel. It re-attained tropical cyclone status on April 5 and reached 10‑minute winds of 160 km/h (100 mph) by the time it made landfall on Mozambique near Pebane, Mozambique on April 8. It dissipated by the next day.
Aside from a tropical disturbance in August, the season began later than usual, the fourth consecutive season to do so. At the time it had the 4th latest start on record for the first named storm. Only about 20% of seasons have their first storm form after the middle of December, and the first named storm of this season, Ando, did not become a tropical storm until early January. However, January was active with three tropical cyclones, two of which became intense tropical cyclones, due to the active phase of the Madden–Julian oscillation (MJO). February returned to a period of inactivity, and generally there was minimal convection across the basin due to unusually dry air. This was spread by a powerful and persistent ridge that extended eastward from Madagascar, as well as an inactive phase of the MJO. Drought conditions occurred on Réunion due to the lack of rainfall. After three weeks of no tropical cyclones developing worldwide, an event unseen since 1995, the tropics became active again in early April.