印度洋季风 meaning in Chinese
indian ocean monsoon
monsoon
Examples
- On the influence of global change of cenozoic climate and uplift of himalayas , the area began to present a distinct seasonal climate on the basis of previous warmth and humidity in pliocene
受新生代全球气候变冷和喜马拉雅运动的影响，该盆地一方面受印度洋季风的影响增强，干湿季节交替明显；另一方面受地形地貌影响，沿袭了温暖湿润的气候条件。 - In winter ( january ) , there are four nearly latitudinal moisture transport belts ( channel ) over asian - australian monsoon region . they are closely related with the easterlies and westerlies over southern hemisphere and northern hemisphere . in boreal winter , asian monsoon region is moisture source ; the cross equatorial moisture transport channels transport the moisture to australian monsoon and south indian ocean from asian monsoon region
主要结论如下： ( 1 )冬季( 1月)的水汽输送形势与南北半球东、西风带紧密联系，主要有四条近似纬向分布的垂直积分的强水汽输送带，越赤道输送将水汽从亚洲季风区输送到南半球澳大利亚季风区和南印度洋季风区，亚洲季风区为水汽源区。 - In july , although the moisture transport from tropical indian ocean reaches its annual maximum to shandong , its contribution to summer rainfall over shandong during july and august is undistinguished . on the other hand , the contribution from sub - tropical west pacific is evident
7月虽然来自热带印度洋季风区的水汽输送通量达到最大值，但7 8月它们对山东夏季降水异常的贡献并不显著，相反来自南海-西太平洋、中国大陆-日本海的水汽输送以及西风带天气系统对山东夏季降水异常的贡献较显著。