1.Effects on Asian Monsoon of Gigantic Qinghai-Xizang Plateau and Western Pacific Warm Pool
Effects on Asian Monsoon of Gigantic Qinghai－Xizang Plateau and Western Pacific Warm Pool
2.over Indochina and Adjacent Monsoon Region
Seasonal Transition of Summer Rainy Season over Indochina and Adjacent Monsoon Region
3.Peculiar Temporal Structure of the South China Sea Summer Monsoon
Peculiar Temporal Structure of the South China Sea Summer Monsoon
4.The East Asian Monsoon Simulation with IAP AGCMs-A Composite Study
The East Asian Monsoon Simulation with IAP AGCMs-A Composite Study
5.Relationships between Regional Indian Summer Monsoon Rainfall and Eurasian Snow Cover
Relationships between Regional Indian Summer Monsoon Rainfall and Eurasian Snow Cover
6.Notice the tie of the ENSO and Indian monsoon, we introduce two ways by which the ENSO affects the East Asian summer monsoon. They are a direct way: ENSO → PJ Pattern → East Asian summer monsoon,and a selective way:ENSO → south Asian monsoon → IEA pattern → East Asian summer monsoon.
气候模式数值试验揭示出印度—东亚遥相关型对东亚很重要并且与印度洋海温异常有关 ,借此提出ENSO影响东亚夏季风的两条途径 :一条是直接路径 ,另一条为选择性路径。
7.The daily monsoon index of Qinghai?Xizang Plateau during 1961—1995 is calculated, the start and end time of summer monsoon of Qinghai?Xizang Plateau are preliminarily determined. Based upon that, we investigate the interannual variation features of the monsoon index and its relationship with the 500 hPa geopotential height fields and monsoon of East Asia.
通过计算 196 1— 1995年逐日青藏高原季风指数 ,初步确定了高原夏季风开始和结束的时间 ,在此基础上研究了季风指数的年际变化特征以及和 5 0 0hPa高度场、东亚季风之间的可能联系。
8.The first was the monsoon onset over the eastern coast of the Bay of Bengal (BOB) in early May. It was followed by the onset of the East Asian monsoon over South China Sea (SCS) by May 20, then the onset of the South Asian monsoon over India by June 10. The BOB monsoon was directly linked to the thermal as well as mechanical forcing of the Tibetan Plateau.
第一阶段是5月上旬在孟加拉湾东岸，称为孟加拉（BOB）季风爆发阶段。 第二阶段是5月20日左右开始的中国南海（SCS）季风爆发阶段。
9.At the same time the strengthened heat low over the ArabianPeninsula also leads to an eastward acceleration of the westerly, so the Indian summer monsoon onset starts on Pentad 31.4. The timing of the stepwise onset and advance of the Asian summer monsoon from 1979 to 2001 is identical to the result from the climatological analysis, indicating that the onset of the tropical eastern Indian Ocean acts as a very important role in onset process of the Asian summer monsoon.
4.1979-2001各年亚洲夏季风的阶段性爆发时间的推进顺序与上述气候学研究结果基本一致,表明热带东印度洋夏季风的建立确实在整个亚洲夏季风建立进程中处于重要的地位。
