南亚季风

南印度洋SST与南亚季风环流年代际变化的研究

Research on interdecadal variability of South Indian Ocean SST and South-Asia monsoon circulation

如果称位于105°E附近的赤道涡旋为东亚的爆发涡旋，它显然与南亚季风的情况有较大差别。

If the 105 ° E equatorial vortex is called onset vortex of East Asia , it is sure that this vortex is different from that of South Asia .

东亚季风和南亚季风的反相位关系及其与ENSO的联系：年际尺度和轨道尺度

Inverse phase between South Asian and East Asian summer monsoons and its relation with enso : from interannual to orbital scale

利用美国NCEP全球大气再分析资料和JONES全球海表面温度异常（SSTa）资料，分析了南印度洋SSTa和南亚季风环流年代际变化的特征。

The NCEP NCAR monthly mean reanalysis data and Jones & Parker 's dataset which is a combination of land air temperature anomalies and sea surface temperature anomalies are used to study the interdecadal variability in South Indion Ocean SST and the South Asia monsoon circulation .

同时11a滑动相关系数也清楚地反映了南亚季风对云南5月强降水天气的影响大于南海季风。

The 11 yeas ' running correlation coefficients also indicate that the effect of the South Asia monsoon on the May heavy rainfall in Yunnan is bigger than that of the South Sea monsoon .

基本流和切变流影响下的南亚季风

South Asia monsoon affected by basic and shear flow

南亚季风区加热影响副高的数值试验

Numerical experiments of the West-Pacific subtropical high influenced by heating in South-Asian monsoon area

东亚季风区和南亚季风区准两年振荡的结构差异

The different Structure in QBO between East Asia Monsoon Region and South Asia Monsoon Region

东亚季风的活动规律及其与南亚季风的区别

The Characteristics of East Asia Monsoon and the Difference between East Asia and South Asia Monsoon

地形和热力效应对南亚季风产生与维持的机理探讨

Toward the Mechanism of Terrain / Thermal Effect and the Production / Maintenance of South-Asia Monsoon

热带海洋对南亚季风和太平洋信风强迫的几种响应模态

Several Response Modes of Tropical Ocean to the Southern Asia Monsoon and the Pacific Trade Wind Forcing

对于全球最显著南亚季风环流的分析表明，南亚季风环流也存在明显的年代际时间尺度的变化。

The study of the South Asia monsoon circulation clearly shows that there is interdecadal variation it .

亚洲南部的季风（下称南亚季风）和亚洲东部的季风（下称东亚季风）一样，都属于海陆季风，主要是由海陆之间的热力差异引起的。

Like the East Asia Monsoon , the Southern Asia Monsoon is also also caused by Thermal difference between sea and land .

然而，东亚季风和南亚季风在本区所起作用的程度以及季风的机制有待进一步的研究。

However , the detail effects of Indian Monsoon and East Asian Monsoon on the plateau and their mechanisms are to be researched .

夏季东亚季风区水汽输送特征及其与南亚季风区水汽输送的差别

Characteristics of the Water Vapor Transport in East Asian Monsoon Region and Its Difference from that in South Asian Monsoon Region in Summer

应用动力学分析和数值计算的方法讨论了热带海洋对南亚季风和太平洋信风强迫的几种响应模态。

By using dynamical and numerical methods , several response modes of tropical ocean to the southern Asia monsoon and the Pacific trade wind forcing are discussed .

用动力分析和数值试验方法研究讨论了地形和热力效应与南亚季风产生和维持的动力机理。

Dynamic and numerical methods are used to study / discuss the mechanism of terrain / thermal effect and the production / maintenance of South Asia monsoon .

研究结果表明，冬季赤道西太平洋环流状况对后期南亚季风和东亚季风以及我国夏季降水均有显著的滞后影响。

The results clearly indi - cate that winter circulation condition over the tropical western Pacific predominantly influences the subsequent South and East Asia Monsoon circulations and summer rainfall in China .

东亚和南亚季风区可降水量的冬夏季节变化最大，夏季的可降水量达冬季值的4倍。

In East and South Asian Monsoon areas have the largest summer and winter seasonal changes of the PW , the PW values summer are four times as large as those winter .

喜马拉雅山毗邻南亚季风区，该地区的地气交换过程也可能受到南亚季风活动的影响。

Besides , the Himalayas is adjacent to the South Asian monsoon regions , the air mass exchange between the surface and free atmosphere could also be affected by the monsoon evolution .

机制的主要内容是：（1）南亚季风系统的双周振荡以澳大利亚高压为启动系统，通过两条途径影响北半球；

Its main opinions are as follows :( 1 ) In southern hemisphere , the oscillations of Australia high not only affect South China sea monsoon trough , but also affect the actions of Mascarene high by propagating westward .

本文通过大量的图表，逐一分析了东亚季风区和南亚季风区准两年振荡的结构差异，得出了一些结论，对于进一步研究东亚季风区和南亚季风区准两年振荡的传播结构起到一些帮助作用。

This paper analyzes the different structure in QBO between east Asia monsoon region and south Asia monsoon region through a lot of charts , gains some conclusion , it can help to study further the propagation structure in QBO between east Asia monsoon region and South Asia monsoon region .

南亚夏季西南季风成因的数值试验研究

Numerical experiment research of the cause of southwest monsoon formation in South Asia

夏半年水汽汇30－60天变化的传播在东亚和南亚两个季风区有不同的特点，这在一定程度上反映了两个季风系统的相对独立性。

The propagational difference of 30-60 day fluctuation over regions of East Asia and South Asia in summer was Found by means of lagged correlation analysis . To some extent , this regional difference indicates the difference of the two Asian monsoon systems .

还计算了南亚地区4～6月的季风指数，分析了云南5月雨量与初夏南亚季风指数变化的关系。结果表明，南亚季风指数高，云南5月雨量偏多；

The relationship between monsoon index from April to June over South Asia and precipitation in May over Yunnan is also studied .

行星风带的季节移动对南亚地区的影响强度受到海陆热力差异的制约，其固有的季节移动作用，对南亚季风形成只起加强的作用。

The seasonal movement of planetary wind system only enhances the formation of the Southern Asia Monsoon , and its effective strenth is conditioned by thermal difference between sea and Land .