西风漂流 meaning in Chinese
antarctic circumpolar current
west wind drift
Examples
- Under perpetual winter condition iap r15l9 agcm is set up for sensitive experiments of pacific ssta without seasonal variability
Iapagcm冬季条件下的敏感性试验表明，大气环流对中纬度西风漂流区与热带中东太平洋持续性ssta均有显著的响应。 - The reverse distributions pattern of ssta over the east pacific region and west wind drift region not only occurs in the summer of severe drought and flood years of north china , but also in the preceding spring
( 3 )赤道东太平洋和西风漂流区相反的海温距平场配置不仅出现在华北夏季严重旱涝年同期，在前期春季也表现得十分清晰。 - Various statistical research reveals that there is significant correlation between north hemisphere circulation and ssta in west wind drift region , as well as in tropical eastern pacific , which are the two key regions in pacific
中纬度西风漂流区以及热带中东太平洋ssta与北半球大气环流存在显著的相关，是太平洋最主要的两个关键区。 - The frequency analysis of area - averaged ssta time series in key regions indicates that the power spectrum peaks is centered at 2 - 4yr annual oscillation , and there is also long temporal scale oscillation such as quasi decadal oscillation revealed by wavelet analysis
时频分析表明，这两个海区区域平均的ssta时间序列存在显著的2 - 4年年际振荡以及准年代际变化。自相关分析表明西风漂流区与热带中东太平洋ssta在冬季的持续性较好。 - The circulation of positive pna index pattern is prominent in the case of persistent forcing of negative ssta in west wind drift region or positive ssta in tropical eastern pacific , which is the typical ssta pattern during el nino peak - mature phase
西风漂流区持续负ssta时或者热带中东太平洋持续正ssta时，阿留申低压均有所加强，正pna指数型的大气环流特征显著。而当相反符号的ssta持续作用时，大气中阿留申低压减弱，对应pna指数为负。