多雨年 meaning in Chinese
rainy year
Examples
- East asia north wind indexes in drought years are larger than in flood years on each levels
各层少雨年东亚北风指数都大于多雨年东亚北风指数。 - ( 2 ) tpnes precipitation anomalies is the highest in northwest china , and the dry years are more than the wet years , whereas no the lasting dry years
( 2 )青藏高原东北侧区是西北地区降水异常最为敏感的区域，其少雨年的概率大于多雨年，但不存在持续少雨年。 - The southern asia high and the subtropical high of the more precipitation years and colder years are both more weak ; the southern asia high and the subtropical high of the more precipitation years and colder years are both more strong
多雨年和凉年的南亚高压和副高都较常年偏弱、少雨年和热年的南亚高压和副高都较常年偏强。 - ( 3 ) the polar eddy , the west circumfluence on 500hpa medium latitudinal region ands subtropic circumfluence are the key systems of tpnes floods precipitation and , the wet years have abundant vapor , moreover , the omga is positive in all atmosphere
( 3 )极涡、中高纬西风环流系统和副热带系统是影响青藏高原东北侧区汛期降水的大尺度环流背景关键系统。同时，多雨年的主要流场特点是有利于水汽输送，且整层大气始终表现为上升运动。 - 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。