高原季风

高原季风对500hPa中纬度西风带活动的影响

The relationships between Plateau Monsoon and 500 hPa Westerly Activities In Mid-latitude

高原季风的年代际振荡及其原因探讨

Discussion on inter-decade oscillation of plateau monsoon and its causes

分析了高原季风强弱年同期和前期SST场、风场和OLR场演变特征。

The evolutionary characteristics of the prophase and synchronous SSTA fields , wind fields and OLR fields are also analyzed .

利用NOAA长波辐射OLR，NCEP/NCAR再分析格点资料，探讨了热带太平洋、印度洋海温等环境场变化与高原季风发展的联系。

By using NOAA OLR data and NCEP / NCAR reanalysis grid data , the relationship of tropical Pacific and Indian Ocean SST background field changes and the development of monsoon over the Plateau are analyzed .

另外，也讨论了高原季风的问题。

In addition , the problem of Plateau monsoon is discussed , too .

高原季风强弱对南亚高压活动的影响

Impact of Strong / Weak Plateau Summer Monsoon on South Asia High Activity

热带海温变化与高原季风发展

Relationship between tropical sea surface temperature change and monsoon development over the plateau

高原季风的平均气候特征

On climatic characteristics of the Xizang Plateau Monsoon

一个新的划分第四纪的标志&高原季风演变的地质环境后果

A new mark for delimitation of quaternary : stable appearance of plateau monsoon and its environmental effects

本文对过去30年来关于高原季风的研究作了一扼要的总结性回顾。

In this paper , the researches of Plateau Monsoons during the past 30 years were described .

一个新的高原季风指数与四川盆地夏季降水的关系

Relationship between a New Plateau Monsoon Index and Summer Precipitation in Sichuan Basin and Analysis of Circulation Features

结果表明：四川盆地初夏干旱的季风环流特征是高原季风偏弱，高原季风低压偏西，我国东部地区东亚季风偏弱，东亚季风槽偏南；

The results are as follows : The characteristics of Plateau monsoon and East Asian monsoon for drought and wet years in early summer are different .

高原季风异常可能与高原下垫面热力异常有关，从而推测冬季风异常通过高原这个巨大的热载体而影响夏季风异常。

It is suggested that the monsoon abnormity in plateau is affected by the special surface thermotics which is the media of winter monsoon abnormity leading to summer monsoon abnormity .

高原季风强年，南亚高压脊线6月北跳比多年平均早1候，8月南撤晚1～2候；

In strong Plateau monsoon year , ridge axis of South Asia high jump to the north in June which is earlier 1 pentad than normal year , and withdraw to south in August which is later 1 or 2 pentads and nearly vice versa .

青藏高原地区季风特征及与我国气候异常的联系

Relationship between Qinghai-Xizang Plateau Region monsoon features and abnormal climate in China

单种属泥炭纤维素碳稳定同位素组成与全新世青藏高原东部西南季风变化把某物埋藏到地底下。

Correlation between Indian Ocean Summer Monsoon and Stable Carbon Isotopic Composition from Mono-species Plant Cellulose in the Holocene ;

青藏高原雪盖与东亚季风异常对华南前汛期降水的影响

The influence of abnormal snow cover over Qinghai-Xizang Plateau and East Asian Monsoon on early rainy season rainfall over South China

结果表明：受不同气候系统影响的西北地区可划分为西风带、高原区与东亚季风等3个气候影响区，水汽沿西北、西方与西南3条路径输送到西北地区；

, region of westerly belt , region of plateau and region of East Asian monsoon . Water vapor is transported from Northwest and West and Southwest to Northwest China .

青藏高原的存在加强了高原东侧的季风，使得季风区向北发展，青藏高原对东亚季风起放大器的作用；

The Qinghai-Xizang Plateau works the East Asian monsoon as an amplifier , makes it strengthen and develop northward .

在青藏高原隆起的整个过程中，高原季风的演化可分为3个阶段，其划分的依据是：高原隆起的水平尺度和垂直高度与高原季风形成所要求的临界尺度之比值。

The development of the Plateau Monsoon may be divided as 3 stages in the entire period of Plateau arising .

高原黄土沉积地层的黄土-古土壤序列中蕴藏着丰富的环境变化信息，是研究高原季风演化的良好地质记录。

Our study also shows that loess paleosol sequence is one of the best sources from which the history of the plateau monsoon evolution can be derived .