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September 14, 1959 ― Typhoon Sarah, known in Japan as the Miyakojima Typhoon, kills 7 and causes US$2 million in damages on Miyakojima. September 26, 1959 ― Typhoon Vera, known in Japan as the Isewan Typhoon, would be the worst typhoon to affect the nation on record, killing 5,098 and causing US$261 million in damages. [17]
The Regional Specialized Meteorological Center (RSMC) for tropical cyclone forecasts is in Japan, with other tropical cyclone warning centres for the northwest Pacific in Hawaii (the Joint Typhoon Warning Center), the Philippines, and Hong Kong. Although the RSMC names each system, the main name list itself is coordinated among 18 countries ...
These typhoons affected Japan. Pages in category "Typhoons in Japan" The following 200 pages are in this category, out of approximately 205 total.
The Northwest Pacific basin covers a vast area in the Pacific Ocean, located north of the equator, between 100°E and 180°E. [1] Several weather agencies monitor this basin, however it is officially monitored by the Japan Meteorological Agency (JMA, RSMC Tokyo), who is responsible for forecasting, naming and issuing warnings for tropical cyclones. [1]
Tropical cyclones that occur within the Northern Hemisphere between the anti-meridian and 100°E are officially named by the Japan Meteorological Agency when they become tropical storms. [2] However, PAGASA also names tropical cyclones that occur or develop into tropical depressions within their self-defined area of responsibility between 5°N ...
Typhoon Hagibis, known in Japan as Typhoon No.19 or Reiwa 1 East Japan Typhoon (令和元年東日本台風, Reiwa Gannen Higashi-Nihon Taifū), [1] was a large and costly tropical cyclone that caused widespread destruction in Japan.
A dangerous weather phenomenon called a bomb cyclone that occurs in mid-latitudes - between Earth's tropics and the polar regions - can bring strong and damaging winds, torrential rains, heavy ...
Cyclones have also been seen on extraterrestrial planets, such as Mars, Jupiter, and Neptune. [7] [8] Cyclogenesis is the process of cyclone formation and intensification. [9] Extratropical cyclones begin as waves in large regions of enhanced mid-latitude temperature contrasts called baroclinic zones.