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The East Asian monsoon is a monsoonal flow that carries moist air from the Indian Ocean and Pacific Ocean to East Asia.It affects approximately one-third of the global population, influencing the climate of Japan, the Korean Peninsula, Taiwan, China, the Philippines and Mainland Southeast Asia but most significantly Vietnam.
Japan is generally a rainy country with high humidity. [1] Because of its wide range of latitude, [1] seasonal winds and different types of ocean currents, [citation needed] Japan has a variety of climates, with a latitude range of the inhabited islands from 24°N – 46°N, which is comparable to the range between Nova Scotia and The Bahamas in the east coast of North America. [1]
Monsoon floods in the Philippines Monsoonal summer thunderstorm in Silang, Cavite, Philippines. The East Asian monsoon affects large parts of Indochina, the Philippines, China, Taiwan, Korea, Japan, and Siberia. It is characterised by a warm, rainy summer monsoon and a cold, dry winter monsoon.
Japan later adapted and transliterated the Chinese term "plum rain" to call the rainy season tsuyu (梅雨). The season is instead commonly called Jangma (장마) in Korea, which means "long rain". The term was originally spelled Dyangmah (댱맣) in 1500s, which was the mix of the hanja character 長 ("long") and the old native Korean word 맣 ...
From May through August, the summer monsoon shifts through a series of dry and rainy phases as the rain belt moves northward, beginning over Indochina and the South China Sea (May), to the Yangtze River Basin and Japan (June) and finally to North China and Korea (July). When the monsoon ends in August, the rain belt moves back to South China.
A monsoon is a shift in seasonal wind pattern that brings on a very rainy period. In the U.S., the desert southwest, the summer monsoon season usually begins around mid-June. This occurs when ...
The highest recorded temperature in Japan was 41.1 °C (106.0 °F) on 23 July 2018. An unverified record of 42.7 °C was taken in Adachi, Tokyo, on 20 July 2004. The high humidity and the maritime influence make temperatures in the 40s rare, with summers dominated by a more stable subtropical monsoon pattern through most of Japan.
In Bengal, abnormal cold and snow was reported in the winter monsoon. [16] In Japan, which was still cautious after the cold-weather-related Great Tenmei famine of 1782–1788, cold damaged crops, but no crop failures were reported and there was no adverse effect on population. [20] Sulfate concentration in ice cores from Greenland.