1942 Pacific typhoon season | |
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Seasonal boundaries | |
First system formed | January 25, 1942 |
Last system dissipated | December 17, 1942 |
Seasonal statistics | |
Total storms | 30 |
Total fatalities | Unknown |
Total damage | Unknown |
Related articles | |
The 1942 Pacific typhoon season has no official bounds; it ran year-round in 1942, 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 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 1942 Pacific hurricane season.
There were 30 tropical cyclones in the western Pacific in 1942. [1] Nine tropical storms are reported in August, which made it the most active August known at the time. [2]
Tropical storm (SSHWS) | |
Duration | January 25 – January 29 |
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Peak intensity | 110 km/h (70 mph) (1-min); |
The storm didn't really affect that much but it affected the Caroline Islands during late-January 1942. [3]
Tropical storm (SSHWS) | |
Duration | April 8 – April 13 |
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Peak intensity | 100 km/h (65 mph) (1-min); |
This storm is very similar to Tropical Storm One. It has the very same track but it is slightly towards the east and affected the Caroline Islands. [4]
Tropical storm (SSHWS) | |
Duration | July 28 – July 30 |
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Peak intensity | 100 km/h (65 mph) (1-min); |
A storm formed north of the Philippines on July 28. It impacted Hainan and southern China on July 29–30, as it was dissipating. [5]
Tropical storm (SSHWS) | |
Duration | December 13 – December 17 |
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Peak intensity | 100 km/h (65 mph) (1-min); |
The final storm of the season developed on December 13 east of Mindanao, Philippines or in the Philippine Sea. It moved in a fast, northward direction. On the 15th, it moved west, and then west the next day. It finally dissipated early on the December 17, due to vertical windshear. [6]
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. It was an event in the annual cycle of tropical cyclone formation. The season had no official bounds, but tropical cyclones in the Western Pacific Ocean normally develop between May and October.
The 1995–96 South-West Indian Ocean cyclone season was a moderately active season that included Cyclone Bonita, which was the first known tropical cyclone to cross from the southern Indian Ocean into the southern Atlantic Ocean. Tropical activity lasted for about six months from the middle of November 1995 to early May 1996. The first storm, Intense Tropical Cyclone Agnielle, formed in the adjacent Australian basin on November 16 and later reached peak winds in the south-west Indian Ocean. The next named storm after Agnielle was Bonita, which formed in early January and killed 42 people. The basin was most active in February, with two tropical cyclones, or the equivalent of a minimal hurricane, as well as a severe tropical storm. The first of these three was Doloresse, which killed 67 people due to a shipwreck in the Comoros. The next storm was Cyclone Edwige, which caused heavy crop damage on Mauritius before looping along the east coast of Madagascar. In March, both Cyclone Flossy and Tropical Storm Guylianne passed near the Mascarene Islands, producing heavy rainfall and gusty winds.
The 1978–79 South Pacific cyclone season ran year-round from July 1 to June 30. Tropical cyclone activity in the Southern Hemisphere reaches its peak from mid-February to early March.
The 1992–93 South-West Indian Ocean cyclone season lasted longer than normal, with the first storm Aviona forming on September 27 and the final storm Konita not dissipating until May 7. It was an above-average season, with four tropical cyclones – the equivalent of a minimal hurricane – along with six tropical storms, one subtropical depression, and several depressions including one that was named. The basin is defined as the area west of 90°E and south of the Equator in the Indian Ocean, which includes the waters around Madagascar westward to the east coast of Africa. Tropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion (MFR), as well as by the Joint Typhoon Warning Center (JTWC).
The 1986–87 South-West Indian Ocean cyclone season was below average due to an ongoing El Niño and a weak monsoon that suppressed convection and storms. There were only five named storms tracked by the Météo-France office (MFR) on Réunion. The United States-based Joint Typhoon Warning Center (JTWC) followed four other storms in the basin, which is the waters of the Indian Ocean south of the equator and west of 90° E to the coast of Africa. The JTWC tracked a storm on August 1 in the northeastern portion of the basin, unusual for the time of year. The first named storm was Severe Tropical Storm Alinina, which originated from the Intertropical Convergence Zone east of Madagascar in the middle of January. However, there was an unnamed tropical depression that produced heavy rainfall in Réunion and Madagascar, causing two deaths in the latter country.
The 1961–62 South-West Indian Ocean cyclone season was a busy cyclone season, lasting from December to April.
The 1940 Pacific typhoon season marked an interruption in meteorological records in both the Philippines and Hong Kong due to the start of World War II. There were 43 reported tropical cyclones, including 27 that attained typhoon status. The first storm was observed in February, and the first typhoon formed two months later, killing three people along Mindanao. Several storms formed in June and July, including reports of a typhoon in the newspapers that killed 52 in South Korea, and another typhoon reported in newspapers that killed one person on Samar after dropping heavy rainfall. The strongest typhoon of the season originated in July and attained a minimum pressure of 927 mbar (27.4 inHg), as reported by a ship northeast of the Philippines.
In 1901, 21 tropical cyclones were observed in the western Pacific Ocean, north of the equator. In that region of the world, cyclones that attain maximum sustained winds of at least 118 km/h (73 mph) are known as typhoons. Out of the 21 storms, the Hong Kong Observatory tracked nine of them. The strongest storm, known as the De Witte typhoon, reached a minimum barometric pressure of 920 mbar (27 inHg), before striking eastern China.
The 1941 Pacific typhoon season has no official bounds; it ran year-round in 1941, 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 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 1941 Pacific hurricane season. There were 28 tropical cyclones in the western Pacific in 1941.
The 1943 Pacific typhoon season has no official bounds; it ran year-round in 1943, 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 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 1943 Pacific hurricane season.
The 1944 Pacific typhoon season has no official bounds; it ran year-round in 1944, 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 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 1944 Pacific hurricane season.
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 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.
The 1938 Pacific typhoon season featured 31 storms. Data from this period was extremely sparse, so intensity is not available for these systems. The only agency that tracked these typhoons is the International Best Track Archive for Climate Stewardship (IBTrACS), which has compiled a database of all known tropical cyclones since 1851.
The following is a list of North Indian Ocean tropical cyclones from 1930 to 1939. Records from before the 1970s were extremely unreliable, and storms that stayed at sea were often only reported by ship reports.
The following is a list of North Indian Ocean tropical cyclones from 1920 to 1929. Records from before the 1970s were extremely unreliable, and storms that stayed at sea were often only reported by ship reports.
The following is a list of South-West Indian Ocean tropical cyclones in the 1950s decade, before the 1959–60 season.
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