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 多雨年发生在enso年和no - enso年大气环流形式的不同主要表现在： enso年副热带高压较强，贝加尔湖地区南部低压槽容易加深；在no - enso年副热带高压强度减弱，在西北太平洋和南海地区多热带系统活动。
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