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baikal lake 貝加爾湖。

bail

The atmospheric circulation of the wet year deviate from enso year to no - enso year . in enso year , the subtropical high is strong with the deepening of trough over south of baikal lake while in no - enso year , the subtropical high is weak with the high incidence of typhoons over northwest of pacific and south china sea 多雨年發生在enso年和no - enso年大氣環流形式的不同主要表現在: enso年副熱帶高壓較強,貝加爾湖地區南部低壓槽容易加深;在no - enso年副熱帶高壓強度減弱,在西北太平洋和南海地區多熱帶系統活動。