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The 1998 Pacific typhoon season was the least active Pacific typhoon season on record, until it was surpassed 12 years later. It would produce 16 tropical storms, 8 strengthening into 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 1993 Pacific typhoon season was the most active season for the Philippines, seeing a total of 32 storms forming or entering their area of responsibility. Overall, it was an average season, spawning 28 tropical storms, 15 typhoons and three super typhoons. The season had 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 1978 Pacific typhoon season was a very active season that produced 31 tropical storms, 16 typhoons and one intense typhoon. 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 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 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 1965 Pacific typhoon season has no official bounds; it ran year-round in 1965, 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 1960 Pacific typhoon season had no official bounds; it ran year-round in 1960, 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 1954 Pacific typhoon season has no official bounds; it ran year-round in 1954, 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.
Typhoon Gordon, known in the Philippines as Typhoon Goring, was a powerful tropical cyclone that caused widespread damage and loss of life in the Philippines and Southern China in July 1989. Gordon developed into a tropical depression near the Northern Mariana Islands on July 9 and quickly intensified as it tracked west-southwestward. On July 13, the storm attained typhoon status and subsequently underwent a period of rapid intensification. By July 15, the storm attained its peak strength as a Category 5 equivalent super typhoon with winds estimated at 260 km/h (160 mph). After striking the northern Philippines, Gordon moved through the South China Sea and slowly weakened. On July 18, the storm made landfall in southern China and was last noted the following day as it dissipated over land.
There were 30 tropical cyclones in the western Pacific Ocean in 1931, including 19 typhoons, as well as one that developed in December of the previous year. The most significant typhoon was one that struck eastern China near Shanghai in the midst of the country's worst floods on record; heavy rainfall caused levees to collapse along the Grand Canal, killing an estimated 300,000 people, including about 2,000 people overnight in the city of Gaoyou.
The following is a list of Pacific typhoon seasons from 1902 to 1919. Data from these years was extremely unreliable, so there were many more typhoons that did not hit land and were not detected by ships.
The following is a list of Pacific typhoon seasons from 1920 to 1935. Data from these years was extremely unreliable, so there were many more typhoons that did not hit land and were not detected by ships. The average from these times was 23 tropical storms, which now would be considered a well-below-average season.
This article encompasses the 1850s Pacific typhoon seasons. The list is very incomplete; information on early typhoon seasons is patchy and relies heavily on individual observations of travellers and ships. There were no comprehensive records kept by a central organisation at this early time.
This article encompasses the 1870s Pacific typhoon seasons. While data is not available for every storm that occurred, some parts of the coastline were populated enough to give data of typhoon occurrences.
This article encompasses the 1890s Pacific typhoon seasons.
References
- ↑ Huang, G; Yim, Wyxx W-S. "Reconstruction of an 8,000-year record of Typhoons in the Pearl River Estuary, China" (PDF). HKU Scholars Hub.
- ↑ "23 Oct 1862 - TERRIFIC TYPHOON IN THE CHINA WATERS, AND IMMENSE LOSS OF LIFE. - Trove". Courier. Trove.nla.gov.au. 23 October 1862. Retrieved 2022-03-26.
- 1 2 3 4 5 6 7 R. García-Herrera; P. Ribera; E. Hernández; L. Gimeno (2010). The Selga Chronology Part I: 1348-1900. Typhoons in the Philippine Islands 1566-1900 (Report). JGR - Atmospheres. Archived from the original on 2021-12-06. Retrieved 2014-07-27.
- 1 2 Kubota, Naoyuki; Matsumoto, Jun; Zaiki, Masumi; Tsukahara, Togo; Mikami, Takehiko; Allan, Rob; Wilkinson, Clive; Wilkinson, Sally; Wood, Kevin; Mollan, Mark (2020). 江戸時代末期に日本近海で外国船に観測された台風 [Tropical cyclones observed by foreign ships near Japan during late Edo era]. 2020年度日本地理学会秋季学術大会 (in Japanese). The Association of Japanese Geographers. doi:10.14866/ajg.2020a.0_104 . Retrieved 2024-06-16.
- ↑ Cox, Samuel J. (July 2021). "H-063-3: The Battle of Shimonoseki Strait, Japan, 1863". Naval History and Heritage Command . Retrieved 2024-06-16.
- ↑ Kusakabe, Masao (December 1961). "史料からみた北海道の気象災害" [A Historical Aspect of Natural Damage in Hokkaidō](PDF). 天気 (in Japanese). 8. The Meteorological Society of Japan: 403–409. Retrieved 2024-07-17.