1) monsoon trough
季风槽
1.
The results suggest that,during the second Meiyu season in 1962,a new ridge is rebuilt in the southern part of WPSH,forming a double ridges process,because of the monsoon trough strengthening and extending eastward,making the WPSH distorting strongly.
结果表明:1962年“二度梅”期间,由于季风槽的加强东伸,副高外围变形,在其南侧新生一条脊线,呈现双脊线结构。
2.
The Asian summer monsoon trough consists of two major components: the South China Sea(SCS) summer monsoon trough and the Indian summer monsoon trough.
亚洲夏季风槽包括两大重要组成部分,即南海夏季风槽和印度夏季风槽。
2) Summer monsoon trough
夏季风槽
3) Indian monsoon trough
印度季风槽
1.
Analysis has been conducted,including,the three dimensional structure of the Indian monsoon trough and the monsoon depression,as well as the vorticity and moisture budgets.
对2003年夏季风期间,7月24~28日印度季风槽内季风低压发展西移与阿拉伯海中尺度低压合并引发南亚的一次大暴雨过程进行了诊断分析,探讨了印度季风槽、季风低压的三维结构以及低压区域的涡度、水汽收支。
4) subtropical summer monsoon trough
副热带夏季风槽
6) Winter monsoon
冬季季风
1.
The results show that(1)the YSWC strength obviously has an interannul variation of 4~7 years period,being well corretated to the longitudinal component of winter monsoon,(2)the YSWC path has a 3～7 years period,obviously influenced by the latitudinal component of winter monsoon,and(3)when the winter monsoon strenthens,YSWC becomes stronger and its path shifts westward.
利用了多年连续的冬季水文调查数据,以黄海暖水舌作为黄海暖流的示性指标,采用经验函数正交分解及相关分析的方法,探讨了黄海暖流的年际变化特征,结果表明:1)黄海暖流的强弱存在4～7a的年际变化周期,并与冬季局地季风的经向分量具有较好的相关关系;2)黄海暖流的流轴存在一个3～6a的变化周期,而且其流轴的摆动明显受冬季季风纬向分量的影响;3)季风增强,黄海暖流增强且流轴西移。
补充资料：季风(见季风气候)
季风(见季风气候)
j!feng候季风见季风气
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条