雨期 meaning in Chinese
rain spell; pluvial
Examples
- The late 1940s - early 1960s and early 1970s to middle 1980s is wet period . the early 1960s to early 1970s is dry period . the significant decrease of rainfall began in the 1990s
40年代末至60年代初期及70年代初期至80年代中期为多雨期， 60年代初期到70年代初期为少雨期， 90年代初期以后又有明显的下降。 - The study on the time series of global land average seasonal precipitation points out that the interannual and interdecadal fluctuations of the rainfall are clear . the late 1940s - late 1960s and the 1980s - 1990s corresponds to wet period and dry period respectively , and the 1970s expresses a apparent interannual variation of rainfall
指出降水有明显的年际和年代际尺度的振荡， 1940s末至1960s末为多雨期， 1980s至今降水多为负距平； 1970s降水的年际变化比较大。 - Result shows that summer precipitation in north china has gone through four major dry - damp phases , richer periods from 1900 to 1915 and from 1946 to 1978 , less periods from 1916 to 1945 and from 1979 to 2001 , and has obvious inter - decadal variations , and has about 60a , 20 - 30a , 10a major periods and has twice abrupt changes in 1953 and 1979
结果表明：华北夏季降水经历了四个主要干湿阶段，即1900 1915年和1946 1978年为多雨期， 1916 1945年和1979 2001年为少雨期，具有明显的年代际变化，主要有约60年、 20 30年和10年左右的周期，并在1953年和1979年发生了两次气候突变。 - Analysis shows that when summer precipitation in north china is richer ( less ) , tropical east pacific ssta is colder ( warmer ) phase , and slp and 500hpa geo - potential height are negative ( positive ) anomaly over the asia , west pacific sub - high is northerner ( southerner ) , and block high in mid - highs latitude happens less ( more ) than normal , east monsoon is stronger ( weaker )
分析表明华北夏季多(少)雨期，赤道中东太平洋ssta处于冷(暖)位相，在非洲大陆上slp利500hpa位势高度均为负(正)异常，西北太平洋副高位置偏北(南) ，中纬度阻塞高压发生频率较低(高) ，东亚夏季风偏强(弱) 。