1) monsoon in Indian Ocean
印度洋季风系统
2) 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。
3) Indian monsoon circulation system
印度季风环流系统
4) 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。
5) 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。
6) Indian summer
印度洋夏季
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