monsoon system

The Stability and Interdecadal Variability of Global Monsoon System

全球季风系统的稳定性与年代际变化

Sensible and latent heat fluxes from the plateau surface are of great importance in the Asian monsoon system .

高原地表的感热和潜热通量在亚洲季风系统中有很重要的作用。

Seasonal mean and low-frequency structures for water transportation in Asian summer monsoon system

亚洲夏季风系统水汽输送的季节平均和低频结构

Dynamic and Moisture Characteristics of Frontal Heavy Rains under Summer Monsoon System over Guangxi

夏季风系统影响下广西锋面型强暴雨动力及水汽输送特征

The two cross-equatorial flows are found to have different influences on the circulation changes related to different members of the Asian summer monsoon system .

两支越赤道气流对亚洲夏季风系统各成员的影响存在明显差异。

Initiation and evolution of the Asian monsoon system timely coupled with the ice-sheet growth and the tectonic movements in Asia

亚洲季风系统的起源和发展及其与两极冰盖和区域构造运动的时代耦合性

Northern Jiangsu basin lies in the transitional region from ocean to continent and its climate is dominated by the East Asian monsoon system .

苏北盆地是我国西部内陆与东部海洋之间的过渡地区，该地区的气候演变历史对揭示东亚季风的时空变化有着重要意义。

There have 46 % national territory in China under the influence of Asian monsoon system , and this area is the gravity of economy 、 culture and politics of China .

我国国土46%左右的地区受到季风气候的影响，而且此区为我国经济、文化、政治的重心地区。

The results , although still preliminary , show that the geographic patterns and the baroclinic structure of global monsoon system are stable , while the monsoon strength undergoes clearly interdecadal variation .

发现全球季风系统的地理分布和斜压结构具有很好的稳定性，但强度存在明显的年代际变化。

The result indicates that the model successfully simulates the monsoon system in the lower troposphere including the classic tropical monsoon , the subtropical monsoon and the temperate-frigid monsoon .

结果表明，模式成功模拟出对流层低层的季风系统，包括经典的热季风以及副热带季风和温寒带季风。

The Cenozoic deformation of Asia was also responsible for the initiation of the Asian monsoon system during the early Miocene and its further strengthening at ~ 8 Ma and ~ 3 Ma .

新生代亚洲形变，也使得亚洲季风系统在早中新世形成，又在约8Ma与约3Ma时强化。

After it first breaks out over the Southeast Asia in the Asian summer monsoon system , summer monsoon over the Southeast Asia affects the peripheral area with varied wind field and convection field .

东南亚地区的夏季风在亚洲季风系统中首先爆发后，通过风场与对流场的变化对周边地区造成影响。

On the other hand , the changes of large_scale vegetation conditions caused by human activities can introduce remarkable influence feedback , a process of importance behaving over the natural variability of the monsoon system .

另一方面，人类活动引起的大范围植被覆盖状况的变化可以对季风气候产生显著的反馈影响，它们是叠加在季风系统自然变率之上的一种重要变化。

Following arguments have been pointed : Mei-yu phenomenon is occurrence in the transition region between the Indian Summer Monsoon System and the trade wind ( or Hadley ) system over the tropical North Pacific ;

东亚梅雨是印度季风体系与北太平洋哈得来（或信凤）体系之间的过渡带中产生的现象；

Since then , the Neogene has witnessed significant variations of the monsoon system , including enhancement of aridity and monsoon intensity at about 15 ~ 13 Ma , around 8 Ma and 3 Ma .

其后，季风系统在晚第三纪又经历了巨大变化，包括15~13Ma前、8Ma、3Ma前干旱气候的加剧和季风系统的加强。

The results show that the diurnal variation of the solar radiation does not have very large influence on the mean monsoon system in the quasi equilibrium state , the main influences may come from the land sea and the topography distributions .

结果表明：准定常的平均季风系统的形势受太阳辐射日变化的影响不明显，其主要的影响可能来自海陆和地形分布。

The new data do not support the onset of the Asian monsoon system around 8 Ma . Rather , the new data led to a hypothesis that the transition to the monsoon climate system in East Asia occurred in the latest Oligocene .

所获得的新资料并不支持亚洲季风系统起源于约8Ma前这一观点，而认为东亚大约是在晚渐新世向季风气候转变这一假设更为合适。

A distinguishing feature of the modern monsoon system is its geographic distribution which disturbs the zonal pattern of indigenous to the planetary climate system , and the appearance of the monsoonal climate pattern in the geological records should signify the onset of the monsoon system .

现代季风系统的一个明显特征，在于它打乱了行星气候系统纬向分布的带状模式，因而地质记录中季风气候地理模式的出现，就应当意味着季风系统的建立。

The glacial-interglacial SST variation in the Japan Sea is considered to be closely related to changes in the East Asian monsoon system , the volume transport of the Tsushima Warm Current ( TWC ) and the position of the sub-polar front ( SPF ) .

日本海海水表层温度的变化主要是与东亚季风、对马暖流的流量、亚极地锋的位置变化等因素密切相关。

It was shown that there exist some remarkable time-delayed correlations in various degree between the Asian summer monsoon system memberships and west Pacific subtropical high index , and they interact and have feedback with each other , playing their own roles in the whole Asian summer monsoon system .

分析结果表明，亚洲夏季风系统成员与西太平洋副高指数之间存在着不同程度的显著时滞相关，各系统成员与西太平洋副高相互作用、互为反馈，构成了亚洲夏季风系统有机的活动整体。

The monsoon circulation system in East Asia and its members are revealed .

揭示出东亚季风环流系统及其成员；

Features and probable mechanism of the medium range variation of east asia summer monsoon circulation system

东亚夏季环流的中期变动特征和可能机制

The interannual variation of Australian high and its effect on the Asia-Australia monsoon circulation system for 1948 & 2002 are analyzed , in the context of NCEP / NCAR reanalysis data .

利用NCEP/NCAR再分析资料，分析了1948&2002年澳大利亚高压（简称澳高，下同）的年际变化及其对亚澳季风环流系统的影响。

As one of the critical members of Asian summer monsoon ( ASM ) system , the diabatic heating of Qinghai-Xizang plateau ( QXP ) plays an important role in the Asian summer monsoon .

青藏高原作为亚洲夏季风系统的主要成员之一，其热力强迫在亚洲夏季风系统中具有重要作用。

The recent discovery of monsoon records in early Miocene raised a question of the time when the East Asian monsoon system initiated .

我国最近发现的早中新世季风记录，对东亚季风系统何时形成又提出了疑问。