Traditional Culture Encyclopedia - Weather inquiry - Climatic characteristics of Japan
Climatic characteristics of Japan
Climate in Hokkaido: Hokkaido is not affected by plum rains, and the rainfall is less than that in other parts of Japan. Summer is short and cool; Winter is long and cold.
Japan's coastal climate: the range is the western coastal area of Honshu Island. Winter is controlled by Siberian high, and the northwest wind blows. At the same time, because the warm current brings a lot of moisture to the horse stream passing through the Sea of Japan in winter, it often snows heavily. There is less precipitation in summer, and sometimes there is abnormal high temperature due to foehn.
Central plateau climate: typical inland climate. It is cold in winter and cool in summer. There is a great temperature difference between winter and summer and day and night. Low rainfall
Pacific side climate: including the east coast of Honshu, Shikoku and most parts of Kyushu. Influenced by the southeast monsoon in summer, there are many strong typhoons in Meiyu period. In winter, there is less snowfall.
Seto Inland Sea Climate: Including Yang Shan, Shikoku, Feng Jingen and parts of Kyushu. The weather here is often sunny, with little rainfall and suffering from drought from time to time.
Climate of Nanxi Islands: The range is Ryukyu Islands. It belongs to subtropical climate, with hot summer and warm winter. Rainstorm. Typhoons often strike in summer.
The precipitation in Japan is the highest in the world. The main reasons include winter snowfall in Japan's coastal areas; Continuous plum rains in June-July (May-June in Okinawa and Amami); And typhoons that landed in or near Japan from summer to autumn. The highest recorded temperature in Japan is 40.9 degrees, which was measured on August 16, 2007 in Kumagaya City, saitama and Tojima City, Gifu Prefecture. The lowest recorded temperature is -4 1 degree, which was 10+degree measured in Asahikawa, Hokkaido on October 25th.
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