1) Asian summer monsoon interstadial/stadial
亚洲夏季风强/弱段
2) Asian summer monsoon
亚洲夏季风
1.
Interannual and interdecadal variations of moisture transport by Asian summer monsoon and their association with droughts or floods in China;
亚洲夏季风水汽输送的年际年代际变化与中国旱涝的关系
2.
Roles of tropical and subtropical land_sea distribution and the Qinghai-Xizang Plateau in the formation of the Asian summer monsoon;
热带、副热带海陆分布与青藏高原在亚洲夏季风形成中的作用
3.
The snow cover on the Tibetan Plateau has obvious seasonal,interannual and interdecadal changes,and is one of the most important factors which control the Asian summer monsoon precipitation.
青藏高原(以下简称高原)积雪具有明显的季节、年际和年代际变化特征,是影响亚洲夏季风降水的重要因子之一。
3) Monsoon year
强弱夏季风
4) strong and weak years of the summer mo nsoon of East-Asia
东亚夏季风强弱年
6) The tropical Asian summer monsoon
亚洲热带夏季风
1.
High-resolution satellite data are used to analyze the features of the onset process of the tropical Asian summer monsoon(TASM) from the point of the climatology view.
利用高分辨率卫星观测资料,从气候态角度分析了亚洲热带夏季风爆发特征。
补充资料：弱风
弱风 弱风 八风之一，指来自东南方的虚风，参“八风”。《灵枢·九宫八风》：“风从东南方来，名曰弱风，其伤人也。内舍于胃，外在肌肉，其气主体重。”
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