印度季风

IOD事件主要通过海洋途径（沿岸开尔文波和印度季风漂流）作用于孟加拉湾，其影响仅局限于湾口一带。

IOD seems to impact the BOB only through oceanic way ( by the coastal Kelvin wave and the Indian monsoon current ), but its influence is only limited to the bay mouth . 3 .

印度季风与东亚夏季环流的遥相关关系

The teleconnection relationship between Indian monsoon and East Asian summer circulation

气候模式虽然有许多限制，不过也的确可以用来模拟许多真实世界的气候现象，例如季节、信风（tradewind）、印度季风（monsoon）等。

Despite their limitations , climate models do capture various aspects of the real world 's climate : seasons , trade winds , monsoons and the like .

指出它们与夏季印度季风环流系统之间存在着密切的联系。

They are closely related with the Indian Monsoon Systems .

印度季风对云南2002年6月6次大到暴雨过程影响分析

Analysis of 6 Yunnan Severe rainfalls affected by Indian monsoon in june , 2002

印度季风低压爆发迟、强度弱；

The India monsoon low deepened eruptively later , and its intensity was weaker .

对喜马拉雅山积雪与印度季风降水呈明显反相关关系的商榷

Comments onan apparent relationship between Himalayan snow cover and summer monsoon rainfall over India

夏季南海季风槽与印度季风槽的气候特征之比较

Comparison of Climate Characteristics Between Two Summer Monsoon Troughs over the South China Sea and India

东亚季风区和印度季风区夏季对流层下部环流的差别与联系

Indian summer discrepancy and relation in the lower tropospheric circulations between the East Asian and Indian monsoons

对印度季风环流系统而言，非洲大陆的影响远大于印度大陆。

For the formation of IMS , the impact of Africa is greater than that of Indian subcontinent ;

夏季印度季风环流系统与我国长江上游区域性持续暴雨的关系

The relationship between Indian monsoon systems in summer and the continuous heavy-rain over upper reaches of the Changjiang

中南半岛对东亚季风环流系统形成起着关键作用，同时对印度季风系统也能产生一定的影响。

Indochina Peninsula not only has key effects on the formation of EAMS , but influences IMS to some extent ;

发现在印度季风爆发的同时，东半球的主要环流系统都有一次相应的突变。

It is found that there is abrupt change in main circulation systems of Asia during the onset of the monsoon .

年平均的负的短波云辐射强迫在中国东部地区明显要大于在印度季风区。

The annual mean negative net cloud radiative forcing in the eastern China is obviously larger than that in the Indian region .

1979年随着印度季风的建立，亚洲季风区上空的水汽输送场经历了非常显著的变化。一条强水汽输送带从阿拉伯海经印度南部、孟加拉湾和南海，然后向北进入华南和日本。

In 1979 , the water vapor transport field over monsoon Asia underwent significant changes with the onset of the Indian summer monsoon .

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。

A diagnostic study is made to investigate the relationship between water vapor transport from Indian monsoon and that over East Asia in Northern summer .

印度季风季来临前，往往是连续多周的强烈光照和气温上升，但像这样危及生命的、高达50度的气温却很不正常。

The run-up to the Indian monsoon season is always characterised by weeks of strong sunshine and increasing heat but life-threatening temperature levels topping 50C are unusual .

石笋记录揭示印度季风的快速推进或退出以及百年尺度上的气候波动是太阳辐射量变化造成的结果。

Stalagmite record revealed that Indian summer monsoon moved forward rapidly , and climate undulation on a century scale resulted in the change of the solar radiation .

通过进一步的诊断，揭示了亚洲夏季风降水在印度季风区出现较晚以及印度夏季风爆发的动力机制。

Further dynamic analysis reveals the dynamic mechanism for the late occurrence of ASM precipitation in Indian monsoon area and the abrupt occurrence of Indian summer monsoon onset .

作为环境驱动力之一的印度季风，对华南特别是云南的气候环境起着重要的作用。

South Asian monsoon , one of the most typical environmental driving force , plays an important role in climate of southern part of China , especially Yunnan province .

理县地区气候演化更接近于印度季风强度记录的变化，而与格陵兰冰心和深海氧同位素记录相似性稍差。

The environmental variations in Lixian County are close to Indian monsoon records in intensity changes , but its similarity to the Greenland Ice Core and deepsea oxygen isotope records is slightly lower .

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；

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 ;

夏季印度季风和东亚季风环流的主要差异之一在于：东亚夏季风环流受中高纬度环流影响很大。

In the paper , It had been pointed out that the main difference between Indian and East Asian summer monsoon is the circulation of mid high latitude had great influence on East Asian Summer monsoon .

印度季风和南海季风在季风爆发的时间上、季风爆发的物理机制上、季风爆发过程中风、温湿场的相互关系上均有明显差异；

The beginning dates , the physical mechanisms of monsoon onset and the relation between wind and temperature or humidity during the onset process in India monsoon region are different from those in South-China sea monsoon region ;

虽然下最终结论为时尚早，但作为亚洲季风的两个组成部分的东亚季风和印度季风很可能是同步的，至少在冰期/间冰期或冰段/间冰段的尺度上是如此。

It is most likely that East Asian and Indian monsoon , as two main components of Asian monsoon , are synchronous , at least , on the timing scale of glacial / interglacial or stadial / interstadial .

本文用天气统计学方法研究了东亚季风区和印度季风区1984年夏半年（5&10月）逐日850百帕流场的时空特征。

Characteristic features of temporal and spatial variations of the flow fields at 850 hPa level over the areas dominated by the East Asian and Indian monsoons during the summer months from May to October , 1984 are analysed by means of synoptic-statistical method .

伴随着冬、夏季节转换，中南半岛以西和以东地区的西风水汽输送的经向移动表现出完全不一样的特征，表明印度季风和东亚-西太平洋季风的形成机制有很大不同。

Further analysis shows that associated with evolving annual cycle , the meridional migration features of westerly moisture transport in areas to the east and west of Indochina Peninsular are quite different , which may also denote different forming mechanisms between the Indian monsoon and East Asian-Western Pacific monsoon .

印度洋季风环流年代际变化及其与大气环流的关系

Interdecadal Variability of Indian Ocean Monsoon Circulation and Its Relation to Atmosphere Circulation

从气候的角度出发，把贵州和印度的季风的某些特征量，如降雨、风、环流等进行对比分析，在一定程度上反映了贵州和印度夏季风的主要异同。

The precipitation , wind and circulation between Guizhou and India are compared and analyzed .

非绝热加热作用对印度西南季风中断向活跃转变过程影响的数值试验

A numerical simulation of diabatic heating effect on transition of Indian southwest monsoon from break to activeness