季风区

中国季风区土壤~（137）Cs背景值研究

Soil ~ ( 137 ) cs background values in monsoon region of China

西北太平洋季风区（5°~25°N，120°~160°E）是亚洲-太平洋季风区与亚洲-澳大利亚季风区的一个重要部分，也是一个独立的季风区。

The monsoon region of western North Pacific ( WNP )( 5 ° - 25 ° N , 120 ° - 160 ° E ) is an important part of Asian-Pacific and Asian-Australian monsoon region , and is a distinct monsoon region .

结果表明，在亚洲季风区内，赤道地区大气动能（K）的最强中心位于75°～90°E，次强中心在索马里急流区（50°E附近）。

Results show that the strongest center of K in the tropical Asian summer monsoon region locates over 75 ° - 90 ° E , with the secondary over Somalia low level jet channel , i.e. , about 50 ° E.

在季风区，对流层下部为季风环流，在非季风区，为Hadley环流；

In the lower troposphere , there are monsoon circulations in the monsoon region and Hadley circulations in the non-monsoon region ;

夏季东亚季风区500hPa月环流异常及其与我国降水关系的向量EOF分析

Vector EOF Expansion of Summer Monthly Anomalous Wind Fields at 500 hPa over East Asia Relation to Rainfall over China

南海季风区有很强的年变化，30～60d和20～30d的变化也比较显著，还有3个月左右的周期变化。

In the area of the SCS monsoon , the annual cycle is very evident , and the oscillations of 30 ~ 60d and 20 ~ 30d are also evident .

对此数据集进行主成分分析（PCA），前2个主成分的时间序列和空间场展示了中国东部季风区植被物候季节性特征和地域差异。

The principle component analysis ( PCA ) was implemented on this data set . The temporal curves and spatial fields of the first and second principle components expose the significant characteristics of vegetation phenology in seasonality and spatial patterns in East China monsoon region .

利用中科院大气所的IAPAGCM-Ⅱ大气环流模式，模拟了在存在和没有赤道东太平洋海温异常影响下，印度洋偶极子对东亚季风区天气气候的影响。

This paper analyses the Indian Ocean Dipole ( IOD ) influence on climate variations over East Asian monsoon region , based on CAS 's IAP AGCM - ⅱ with Equator East Pacific SSTA influence on or not .

北太平洋中、西部副高在北进期的脊线活动均存在显著的10～20d周期低频振荡，东亚季风区还具有明显的准40d振荡周期。

The ridge movement has 10 ~ 20-day low-frequency oscillation during its northward over central and western Pacific , particularly in East-Asian monsoon area with quasi-40-day oscillation period .

分析表明，近赤道季风区显著低频振荡是ELNino发生发展的一个重要前兆，低频振荡能量向甚低频段的转移和输送可能是ELNino发生的一个重要机理。

It is also indicated that the notable ISO is an important auspice for the occurrence and the development of El Nino . The process of low frequency transition to the lower frequency fluctuation energy is an important mechanism associated with the occurrence of El Nino .

澳洲大陆北部的冷性高压，西太平洋副热带高压西端位置西伸或东缩造成的东中国海季风区上升运动的变化，又是南北半球环流同时影响CEF变化的具体表现。

The Australia anticyclone and the west part of the Subtropical anticyclone in the Western Pacific ( Eastern China Sea monsoon region ) are the indication of the joint impact of Southern and Northern Hemisphere circulation on CEF .

秋季亚洲季风区范围最大的强水汽源地位于南海、西太平洋地区（115～120oE，15～25oN）。

In Autumn , the strongest water vapor source lies in the South China Sea and the west Pacific Ocean , in the region of 115 ~ 120oE , 15 ~ 25oN .

在此基础上，对于选定的最佳模拟区域和侧边界条件，进行嵌套和水平分辨率影响试验，以研究CWRF对中国东部季风区降水模拟宜采用的方案。

On the basis of the decided model domain and lateral boundary conditions , the experiment of nesting and horizontal grid spacing are conducted to study the scheme of CWRF application in East China .

亚洲季风区云和降水的日变化特征分析

Diurnal Characteristics of Cloudiness and Precipitation over the Asia Monsoon Region

亚澳季风区大气视热源的季节演变特征

Seasonal Variability of Atmospheric Heat Sources over the Asian-Australian Monsoon region

东亚季风区夏季风强度和降水的配置关系

The Configurable Relationships between Summer Monsoon and Precipitation over East Asia

梅雨异常与季风区大尺度环流异常的探讨

Relationships between anomalies of Meiyu and large scale circulation in monsoon area

亚澳季风区水汽输送的气候特征

Climatological Characteristics of Water Vapor Transport over Asian - Australian Monsoon Region

中国东部季风区1961年～2006年年平均气温变化特征

The Change of Annual Mean Temperature in Monsoon Area of East China

它们的分布型为季风区型或北方型。

Their distribution type is the monsoon district type and northern type .

南海季风区地域性大气环流的结构

Structure of Regional Atmospheric Circulation in the South China Sea Monsoon Region

东亚季风区植被-大气相互作用研究；

Study of vegetation-climate interaction in East Asia Monsoon region ;

海陆热力差指数能较好地反映东部季风区夏季降水的异常状况。

The index also can reflect summer rainfall anomaly over eastern China .

东亚季风区的极端气候事件及其原因

Pleistocene climate extremes in East Asia and their causes

中国东部季风区末次冰期以来古气候模拟

Simulations of paleoclimate in the East China monsoon area since the last glaciation

亚洲季风区地面感热通量的区域变化特征

Characteristics of spatial variation of surface sensible heat flux in Asian monsoon region

用气象卫星对东亚季风区的生态过渡带的遥感监测研究

Monitoring the ecological transect in East Asia monsoon region by meteorological satellite remote sensing

我国热带季风区的林-胶-茶生态模式

The " trees-rubber - tea " ecological model in the Chinese tropical monsoon region

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

亚洲季风区铁杉属现代分布区及其气候特征

Modern Geographical Distribution of Tsuga and Its Climatic Conditions in the Asian Monsoon Region