The 1996 Pacific typhoon season has no official bounds; it ran year-round in 1996, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.[1] These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1996 Pacific hurricane season. Tropical Storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions in this basin have the "W" suffix added to their number. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names, like Herb or Sally.
On February 23, a large area of convection developed south of the Philippine Sea. The convection developed into a low pressure area and was at first bombarded by wind shear, but conditions soon turned favorable which allowed it to strengthen rapidly on February 27 before becoming a Tropical depression later that day. The JMA upgraded 01W into a Tropical Storm before it drifted over the Philippines on February 29, and weakened slightly due to land interaction.[2][3]On March 1, a cold front brought cold, dry air and vertical wind shear which pushed the system south caused the system's low level circulation center to become exposed. The exposed remnants of 01W continued to drift south, before being completely absorbed by the Intertropical Convergence Zone.[citation needed]
Cam developed over the South China Sea on May 18. The cyclone headed northeastward to east-northeastward and dissipated over the Pacific Ocean on May 23.
A Tropical Upper Tropospheric Trough spawned Tropical Depression 7W on July 10 over the open Western Pacific. It tracked generally west-northwestward, strengthening to a tropical storm on the 14th. On the 15th Eve became a typhoon, which was followed by a period of explosive deepening to a 100mph Typhoon, with a pressure drop of 40 mb from early on the 15th to early on the 16th. An eyewall replacement cycle weakened Eve to a 95mph typhoon, but as the outer eyewall contracted, the storm again reached wind speeds of 97mph before hitting southern Japan on the 18th. Rapidly weakening over the mountains, Eve turned eastward over the islands and the last warning was issued on the 20th. It restrengthened to a tropical storm east of Japan, and continued northeastward until dissipation on the 27th. Eve, despite being a Category 4 at landfall, caused no reported deaths and only 9 injuries.[4]
An active monsoon trough over the Western Pacific Ocean developed 3 typhoons; Frankie, Gloria, and Herb. The first, Frankie, developed in the South China Sea on July 19. It tracked west-northwestward and became a tropical storm on the 21st. After crossing the island of Hainan Frankie rapidly intensified to a 100mph typhoon, 945millibar over the Gulf of Tonkin. It northern Vietnam on the 23rd, and dissipated 2days later over China. 104people were reported killed or missing in association with Frankie,[4] and damage figures in Vietnam are estimated at over 16.65 trillion (US$1.4billion) (1996 US Dollars).[5]
The same monsoon trough that spawned Frankie also spawned a tropical depression on July 19 east of the Philippines. It headed northwestward, slowly organizing into a tropical storm on the 22nd. The next day Gloria reached typhoon strength, and a day later it reached its peak of 100mph winds. Gloria brushed the northern coast of the Philippines and turned northward to hit Taiwan on the 26th. After crossing the island and the Taiwan Strait, Gloria hit China where she dissipated on the 27th. Gloria caused 23 casualties, 20 of which were in the northern Philippines. In addition, damage was estimated at $20million (1996USD).[4]
Super Typhoon Herb was the strongest and the largest storm of 1996. Herb struck Ryūkyū Islands, Taiwan and China. Maximum sustained winds of the cyclone reached 160 miles per hour (260km/h) over the open ocean. The system led to 590 casualties and US$5billion in damage (1996dollars).[4]
A monsoon depression developed on July 28 over the open Pacific Ocean. It headed northwestward, slowly consolidating to become a tropical storm on the 5th. While south of Japan, Kirk drifted to the southeast and looped back to the west, strengthening to a typhoon on the 8th while looping. It continued slowly northwestward, and while curving to the northeast Kirk reached a peak of 110mph winds. The typhoon struck southwestern Japan at that intensity on the 14th. It weakened over the country, and dissipated on the 16th over the northern Pacific. Kirk caused heavy flooding, resulting in at least 2 deaths and moderate damage.[4]
The monsoon trough spawned a tropical depression over southern China on August 11. It drifted southwestward, entering the Gulf of Tonkin on the 12th. An extremely small cyclone, it reached tropical storm strength on the 13th and a peak of 60mph on the 14th. Marty made landfall on the 14th on northern Vietnam, where it dissipated 3days later. Though small and somewhat weak, Marty managed to cause moderate damage and flooding, amounting to the deaths of 125 with 107people missing.[4]
Niki developed on August 16. It struck Luzon on August 19 and then crossed the South China Sea. The typhoon later made landfall in Hainan on August20 and northern Vietnam on August21. Niki dissipated by August23.
On September 2, a tropical depression developed well east of the Philippines. It headed west-northwestward, reaching tropical storm strength on the 5th and typhoon strength on the 6th. On the 7th Sally rapidly intensified to a 160mph Super Typhoon while passing just north of the Philippines. It weakened slightly yet steadily to a 115mph typhoon over the South China Sea, hitting the Luichow Peninsula of China on the 9th, and dissipated the next day over the country. Sally brought heavy rain and damage to China, causing 114 casualties, 110people missing, and economic losses estimated at $1.5billion (1996USD).[4]
Ningning developed on September 6. It struck Luzon on September 9 and then entered the South China Sea. Ningning dissipated offshore Vietnam on September14.
An active monsoon trough that also developed Typhoons Tom (25W) and Violet (26W) spawned a tropical depression in the Gulf of Tonkin on September 16. It moved counter-clockwise around Hainan Island, becoming a tropical storm on the 17th and a typhoon on the 19th. It crossed the narrow Hainan Strait between Hainan and China, and continued west-southwestward across the Gulf of Tonkin. Willie made landfall on Vietnam on the 22nd, and dissipated the next day. The typhoon resulted in 38 fatalities from flooding.[4] Damage in Vietnam reached over 500 billion dong (US$40 million, 1996 dollars).[5]
Beth developed on October 13. It struck Luzon on October 17 and then reached the South China Sea. On October 21, Beth moved ashore in Vietnam and dissipated the next day. One person had drowned in northern Philippines, in the province of Ifugao, while another four remained missing in another province. The PAGASA recorded sustained winds of 120km/h (75mph) as the storm impacted the northeastern portion of Cagayan.[7][full citation needed]
Tropical Depression 34W formed over the Sulu Sea on October 24. It struck Palawan on the next day. After tracking across the South China Sea, 34W made landfall in Thailand on October 30. It crossed the Malay Peninsula and entered the North Indian Ocean basin later that day. The storm dissipated shortly thereafter, but later re-developing into the Andhra Pradesh cyclone.
A cluster of thunderstorm activity formed southeast of Guam on November 2. The system slowly organized, becoming a tropical depression on November 4. Remaining nearly stationary, the depression intensified into a tropical storm late in the day. The cyclone then turned westward, becoming a typhoon by November 7. Late in the day, Dale passed south of Guam bringing winds as high as 74 knots (137km/h) and high seas which overtopped cliffs 30 metres (98ft) high. Damage on the island totaled US$3.5million (1996 dollars.) Continuing to intensify, Dale became a supertyphoon in the Philippine Sea on November 9. On November 10, Dale turned north, recurving east of the Philippines. On November 14, Dale accelerated east-northeast at more than 60 knots (110km/h) as it became an extratropical cyclone.[4]
A tropical depression formed on December 21, when a low-level circulation center began to produce deep convection. The depression strengthened into a tropical storm the next day, and was given the name Fern by the Joint Typhoon Warning Center (JTWC). The storm slowly intensified into a Category 1 typhoon on the Saffir–Simpson hurricane wind scale, according to JTWC. Fern peaked north of Yap on December 26, with JTWC assessing winds of 150km/h (90mph), while the Regional Specialized Meteorological Center, Japan Meteorological Agency (JMA) assessed peak winds of 110km/h (70mph), just below typhoon strength. The storm soon became sheared and weakened slowly. Fern continued to weaken to a tropical depression on December 30. Both agencies stopped advisories later on the same day.
Two active monsoon troughs that also developed Typhoon Fern and Southern Hemisphere Cyclones Ophelia, Phil, and Fergus spawned Tropical Depression 43W in the South China Sea on December 21. Due to the troughs' nature, the depression headed east-southeastward, where it strengthened into the final tropical storm of the year on the 24th; Greg. After reaching a peak of 45 knots (83km/h) winds it crossed the northern part of Borneo on the 25th. It continued east-southeastward until dissipation on the 27th, south of the Philippines. Greg caused extensive property damage on Borneo from torrential flooding, resulting in 127 deaths and 100people missing.[4]
During the season 30 named tropical cyclones developed in the Western Pacific and were named by the Joint Typhoon Warning Center, when it was determined that they had become tropical storms. These names were contributed to a revised list which started in 1996.
Ann
Bart
Cam
Dan
Eve
Frankie
Gloria
Herb
Ian
Joy
Kirk
Lisa
Marty
Niki
Orson
Piper
Rick
Sally
Tom
Violet
Willie
Yates
Zane
Abel
Beth
Carlo
Dale
Ernie
Fern
Greg
Philippines
Asiang
Biring
Konsing
Ditang
Edeng
Gloring
Huaning
Isang
Lusing
Maring
Ningning
Osang
Paring
Reming
Seniang
Toyang
Ulpiang
Welpring(unused)
Yerling(unused)
Auxiliary list
Apiang(unused)
Basiang(unused)
Kayang(unused)
Dorang(unused)
Enang(unused)
Grasing(unused)
The Philippine Atmospheric, Geophysical and Astronomical Services Administration uses its own naming scheme for tropical cyclones in their area of responsibility. PAGASA assigns names to tropical depressions that form within their area of responsibility and any tropical cyclone that might move into their area of responsibility. Should the list of names for a given year prove to be insufficient, names are taken from an auxiliary list, the first 10 of which are published each year before the season starts. Names not retired from this list will be used again in the 2000 season. This is the same list used for the 1992 season. PAGASA uses its own naming scheme that starts in the Filipino alphabet, with names of Filipino female names ending with "ng" (A, B, K, D, etc.). Names that were not assigned/going to use are marked in gray.
Season effects
This table summarizes all the systems that developed within or moved into the North Pacific Ocean, to the west of the International Date Line during 1997. The tables also provide an overview of a systems intensity, duration, land areas affected and any deaths or damages associated with the system.
The 2004 Pacific typhoon season was an extremely active season that featured the second-highest ACE ever recorded in a single season, second only to 1997, which featured 29 named storms, nineteen typhoons, and six super typhoons. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2004, though most tropical cyclones typically develop between May and October. The season's first named storm and also the first typhoon, Sudal, developed on April 4, later was reached typhoon status two days later, and became the first super typhoon of the year three days later. The season's last named storm, Noru, dissipated on December 21.
The 2002 Pacific typhoon season was a slightly above average Pacific typhoon season, producing twenty-six named storms, fifteen becoming typhoons, and eight super typhoons. It had one of the highest ACE of any season worldwide, with over 400 units. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2002, though most tropical cyclones typically develop between May and October. The season's first named storm, Tapah, developed on January 11, while the season's last named storm, Pongsona, dissipated on December 11. The season's first typhoon, Mitag, reached typhoon status on March 1, and became the first super typhoon of the year four days later.
The 2001 Pacific typhoon season was the fourth and final consecutive year with below-average activity, making it the lowest four-year period of activity since 1976–1979, due to the presence of a strong La Niña that had persisted from 1998 to 2001. However, it was more active than the previous seasons, producing twenty-five named storms, sixteen typhoons and three super typhoons, with a near normal Accumulated Cyclone Energy (ACE) of 307.3 units. It ran year-round in 2001, with most tropical cyclones in the northwestern Pacific Ocean tending between May and November.
The 2000 Pacific typhoon season marked the first year using names contributed by the World Meteorological Organization. It was a rather below-average season, producing a total of 23 tropical storms, 13 typhoons and 4 intense typhoons. The season ran throughout 2000, though typically most tropical cyclones develop between May and October. The season's first named storm, Damrey, developed on May 7, while the season's last named storm, Soulik, dissipated on January 4 of the next year.
The 1998 Pacific typhoon season was at the time the least active Pacific typhoon season on record, until the record was surpassed 12 years later, spawning 16 tropical storms and 8 typhoons. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the international date line. Storms that form east of the date line and north of the equator are called hurricanes; see 1998 Pacific hurricane season. Tropical Storms formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions in this basin have the "W" suffix added to their number. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.
The 1997 Pacific typhoon season was a record-breaking season featuring 11 tropical cyclones reaching super typhoon intensity, tying the record with 1965 with the most violent tropical cyclones globally. It has no official bounds; it ran year-round in 1997, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1995 Pacific typhoon season occurred all year round, unusual in that most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November.
The 1993 Pacific typhoon season has no official bounds; it ran year-round in 1993, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1992 Pacific typhoon season had no official bounds; it ran year-round in 1992. Despite this, most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1987 Pacific typhoon season has no official bounds; it ran year-round in 1987, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical storms formed in the entire west pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.
The 1980 Pacific typhoon season has no official bounds; it ran year-round in 1980, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. Tropical storms which formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.
The 1979 Pacific typhoon season featured the largest and most intense tropical cyclone recorded globally, Typhoon Tip. The season also experienced slightly above-average tropical cyclone activity. The season had no official bounds; it ran year-round in 1979, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1978 Pacific typhoon season was a very active season that produced 31 tropical storms, 16 typhoons and one intense typhoon. It has no official bounds; it ran year-round in 1978, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1959 Pacific typhoon season was regarded as one of the most devastating years for Pacific typhoons on record, with China, Japan and South Korea sustaining catastrophic losses.
The 1976 Pacific typhoon season has no official bounds; it ran year-round in 1976, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1970 Pacific typhoon season has no official bounds; it ran year-round in 1970, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1974 Pacific typhoon season was the first season on record to not feature a Category 5 equivalent super typhoon; a feat later repeated by the 1977 and 2017 seasons. Even so, the season was overly active, with 32 tropical storms and 16 typhoons being developed this year. It has no official bounds; it ran year-round in 1974, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1972 Pacific typhoon season was an above average season, producing 31 tropical storms, 24 typhoons and 2 intense typhoons. It has no official bounds; it ran year-round in 1972, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1957 Pacific typhoon season has no official bounds; it ran year-round in 1957, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The 1981 North Indian Ocean cyclone season was part of the annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. 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 Joint Typhoon Warning Center (JTWC) releases unofficial advisories. An average of five tropical cyclones 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.
This page is based on this Wikipedia article Text is available under the CC BY-SA 4.0 license; additional terms may apply. Images, videos and audio are available under their respective licenses.
