太平洋反气旋 meaning in English

pacific anticyclone
pacific high

Based on this conclusion , the possibly formation mechanism of the double sh ridges is discussed . the results show that the formation process of double sh ridge is discrepant for the different style . the first style occurs as a result of the northward movement , the through - get and consolidation of the equatorial buffer band with the wpsh , and the second one is due to the strength , western extension , and then through - get and consolidation of the mid - pacific with the equatorial buffer band
在此基础上，分析了副高双脊线的形成原因，结果表明，不同类型的双脊线，其形成过程不同:第一类双脊线是赤道缓冲带(赤道反气旋)北上与副高打通合并的结果，而第二类双脊线却是由于中太平洋反气旋加强西伸，与赤道缓冲带打通合并而形成的。