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Effects of the El Niño–Southern Oscillation in the United States : ウィキペディア英語版 | Effects of the El Niño–Southern Oscillation in the United States
The El Niño–Southern Oscillation affects the location of the jet stream, which alters rainfall patterns across the West, Midwest, the Southeast, and throughout the tropics. The shift in the jet stream also leads to shifts in the occurrence of severe weather, and the number of tropical cyclones expected within the tropics in the Atlantic and Pacific oceans affected by changes in the ocean temperature and the subtropical jet stream. The winter will have a negative phase according to the Arctic oscillation (AO).〔 ==Temperature== During El Niño, the northern tier of the lower 48, as well as southern Alaska, exhibits above normal temperatures during the fall and winter, while the Gulf coast experiences below normal temperatures during the winter season.〔Climate Prediction Center. (Average October-December (3-month) Temperature Rankings During ENSO Events. ) Retrieved on 2008-04-16.〕〔Climate Prediction Center. (Average December-February (3-month) Temperature Rankings During ENSO Events. ) Retrieved on 2008-04-16.〕
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「Effects of the El Niño–Southern Oscillation in the United States」の詳細全文を読む
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