1) Indian monsoon
印度季风
1.
The characteristics of the Indian monsoon:Evidences from the sedimentary records of Tengchong and Shangri-La over the past 60 ka
从腾冲和香格里拉沉积记录看60ka BP以来的印度季风活动特征
2.
A diagnostic study is made to investigate the relationship between water vapor transport from Indian monsoon and that over East Asia in Northern summer.
诊断分析了北半球夏季来自印度季风的水汽输送与东亚上空水汽输送的关系，发现二者之间具有反相变化的特征。
3.
The progressive analysis shows that the transfers in different stages of the Indian monsoon and the south China sea monsoon are also different, which is also the same as the varying of vapour transferring pe.
进一步分析结果表明，在印度季风和南海季风不同的位相阶段，孟加拉湾地区和南海地区的经向水汽输送也是各不相同的，这也和各月经向水汽输送变化基本一致。
2) Indian summer monsoon
印度季风
1.
With the onset and withdrawal of the Indian summer monsoon,the wind and moisture fields generally show abruptly seasonal transitions,which can be taken as criteria to distinguish the summer monsoon from the winter monsoon.
印度季风区是世界上季风现象最显著的地区,伴随着夏季风爆发和撤退,季风区的大气风场和湿度场都存在明显的季节转换,这种季节转换可以作为区分夏季风与冬季风的一个很好的标准。
3) Indian summer monsoon
印度夏季风
1.
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.
The analysis of 43-year NCEP-NCAR reanalysis data and the station observations reveals the correlation between troposphere temperature variations and the weakening of the Indian summer monsoon circulation.
对43aNCEP/NCAR再分析资料和台站实际观测资料的分析,揭示了对流层温度变化和印度夏季风环流减弱之间的联系。
3.
The interdecadal variation of Indian summer monsoon and the climate shift in North China are analyzed by using of NCEP-NCAR reanalysis data and the stations observations.
利用NCEP/NCAR再分析资料及台站实测资料分析了近几十年印度夏季风的年代际变化特征及我国北方所发生的气候变化,揭示了印度夏季风的减弱与我国北方地区的气候演变具有密切的联系。
4) 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。
5) Indian winter monsoon
印度冬季风
1.
1 and the distributions of heat source calculated by NCEP/NCAR(version 1) reanalysis datasets,the impact of atmospheric cold(heat) source distribution over Asia and the Southern Hemisphere in January on East Asian winter monsoon and Indian winter monsoon are investigated.
1模式及NCEP/NCAR(version 1)再分析资料计算出来的几种现实大气热源分布情况,分别讨论亚洲各地区和南半球上空冬季1月份大气冷(热)源对东亚冬季风环流系统和印度冬季风环流系统形成的影响。
2.
The impact of atmospheric cold(heat) source distribution over Asia and the Southern Hemisphere in January on the East Asian winter monsoon and Indian winter monsoon is simulated with the NCAR CAM3.
1模式及NCEP/NCAR(version 1)再分析资料计算了几种现实大气热源分布情况,讨论了亚洲各地区和南半球上空冬季1月大气冷(热)源对东亚冬季风环流系统和印度冬季风环流系统形成的影响。
6) Indian monsoon system
印度季风系统
1.
Africa and Indian subcontinent) with 90° E as the divide, as well as the subplanetary land-sea distribution over southern Asia on the formation of the Indian monsoon system (IMS) and east Asian monsoon system (EAMS), the major conclusions being summarized as follow.
(3) 孟加拉湾夏季强降水和西南季风以及冬季东北风的形成是印度半岛和中南半岛存在联合造成的,并且二者作用相当,亦即孟加拉湾季风形成是东亚和印度季风系统联合影响结果。
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