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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Climate of Asia ： ウィキペディア英語版 Climate of Asia The Climate of Asia is wet across southeast sections, and dry across much of the interior. Some of the largest daily temperature ranges on Earth occur in western sections of Asia. The monsoon circulation dominates across southern and eastern sections, due to the presence of the Himalayas forcing the formation of a thermal low which draws in moisture during the summer. Southwestern sections of the continent are hot. Siberia is one of the coldest places in the Northern Hemisphere, and can act as a source of arctic air masses for North America. The most active place on Earth for tropical cyclone activity lies northeast of the Philippines and south of Japan, and the phase of the El Niño-Southern Oscillation modulates where in Asia landfall is more likely to occur, ==Temperature== The Southern sections of the continent are warm to hot, while far northeastern areas such as Siberia are very cold. East Asia has a temperate climate. The highest temperature recorded in Asia was at Tirat Tsvi, Israel on June 21, 1942. West-central Asia experiences some of the largest diurnal temperature ranges on Earth. The lowest temperature measured was at Verkhoyansk and Oymyakon, both in Sakha Republic of Russia on February 7, 1892 and February 6, 1933 respectively.〔(Global Measured Extremes of Temperature and Precipitation. ) National Climatic Data Center. Retrieved on 2007-06-21.〕 Between 1871 and 2000 India suffered 22 drought years.〔Ramesha Chandrappa, Sushil Gupta, Umesh Chandra Kulshrestha, Climate Change: Principles and Asian Context, Springer-Verlag, 2011〕 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Climate of Asia」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.