季风

那个地区主要以季风气候为主要气候类型。

The main climate type in that region is monsoon .

撤离灾区涉水通过后在白沙瓦沉重的季风降雨在周六，2010年7月31日

Evacuees wade through flooded area following heavy monsoon rains in Peshawar on Saturday , July 31 , 2010 .

海岸线在另外两个方面大大地影响季风

The coastline significantly influences the monsoons in two other respects .

第一循环（6月初7月中旬），季风降水和西风等都主要位于5°N10°N之间。

In the first cycle ( early June - mid July ), precipitation and west wind mainly locate between 5 ° N - 10 ° N.

150°E&170°W之间为季风环流与信风环流的连接区或过渡区。

From 150 ° E to 170 ° W lies a region of joining or transition between the monsoon and trade circulation .

关于季风动力学以及季风与ENSO循环相互作用的研究

Studies on the Monsoon Dynamics and the Interaction between Monsoon and ENSO Cycle

ENSO对其后东亚季风活动影响的GCM模拟研究

Numerical simulation of the ENSO influences on East-Asian monsoon activities afterwards

亚洲季风与ENSO循环的相互作用

Asian Monsoon and ENSO Cycle Interaction

其中，季风槽的异常偏西及在盛夏的异常偏北对TC的异常活动产生了主要影响。

And in which the anomalous westward and northward movements of monsoon trough in midsummer exerted a main effect on the TC anomalous activities .

拉萨降水中δ18O也表现出季风降水的典型特征。

δ 18 O in summer precipitation has a clear signal of monsoon precipitation .

在不同的SST年代际背景下，东亚季风和ENSO事件的关系是不同的。

The relationship between the east Asian monsoon ( EAM ) and ENSO events is different on the different interdecadal background in SST fields .

黄土高原和南海陆架古季风演变的生物记录与Heinrich事件

Paleomonsoon evolution and Heinrich events : evidence from the Loess Plateau and the South China Sea

分析了赤道地区纬向风的年际变化特征，以及亚澳季风与ENSO在各个位相的联系。

The interannual variability of tropical zonal wind and the relationship between ENSO and the Asian / Australian monsoon in different phases are discussed .

南海季风爆发期SST异常特征及其与风场的关系

Anomalous Characteristics of SST Variations in SCS and the Bay of Bengal during the onset of the SCS summer monsoon and related with the Lower Southwest Air Current

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 ;

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 .

运用小波分析方法和相关分析对东亚季风的准两年振荡（QBO）的存在及其与ENSO变率的关系进行了研究。

In the context of wavelet technique and coherence analysis the existence of east Asian monsoon QBO is investigated together with its relation to ENSO variability .

结果表明，由于SSTA在大气中强迫激发出了大气低频振荡，使得ENSO对其后的东亚季风活动仍有明显影响。

The results show that the influences of ENSO on the afterward monsoon activities in East Asia are in existance owing to atmospheric low frequency oscillation excited by SSTA .

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

而准2a振荡（QBO）则主要与印度洋海洋-季风系统的低频振荡和东亚大槽的强度变化有关，并且都表现为最大滞后相关关系。

QBO is related to the variation of the Indian Ocean-monsoon system and the East Asian trough , which is always shown as a maximum lag correlation .

尤其是台风南部来自SW－S－SE方向的季风汇合带云带，不仅意味着台风强度的加强和维持，更预示着台风将往北移动。

Especially , the long cloud bands of the monsoon confluent zone coming from SW-S-SE direction not only means that typhoon would intensify or maintain its intensity , but also predicts that typhoon would move northward .

南海季风的爆发与20～30d和30～60d两种低频振荡有关。

The onset of the SCS monsoon is the result of the interaction between the low frequency oscillations of 20 ~ 30d and 30 ~ 60d .

西太平洋副高南侧、亚洲季风槽北侧的东南风水汽输送在夏季可向西扩展到甘肃东南部地区（100°E附近）。

The southerly water vapor can progress to 50 N near North-East in China - , the southeasterly water vapor from south side of the west pacific subtropical high and north side of the monsoon trough can march westward to 100 E near south-east part of GanSu in summer .

根据FGGE-ⅡB资料，利用有限区域中准Lagrange坐标的扰动动能方程计算了发生在1979年的两个南海季风低压的扰动动能收支。

In this paper , we calculated the perturbation-kinetic energy budget for two monsoon depressions over the South China Sea which occurred in 1979 , by using FGGE - ⅲ B data and the equation of the perturbation-kinetic energy in a quasi-Lagrange coordinate over a limited area .

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 .

指出了青藏高原感热驱动气泵（SHAP）在调制东亚季风及全球气候中的重要作用；

The importance of the Sensible Heat driven Air Pump ( SHAP ) over the Qinghai Xizang Plateau in regulating the East Asian monsoons and global climate is emphasized .

季风边缘区封闭湖泊近40a来的水位变化分析&以青海湖、岱海为例

Analysis on Water Level Change of Closed Lakes in Fringe of the East Asian Monsoon Area & A Case Study of Qinghai Lake and Daihai Lake

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 .

不同林型间的N2O通量差异与森林土壤的性质有密切关系，C/N比值较低的季风林凋落叶对土壤中产生N2O的微生物过程有较为明显的促进作用；

The difference of N2O flux among the different forests had close correlation with their soil properties ; litter in the monsoon forest of lower C / N ratio had more obvious promotion action on the microbe process of N2O production in soil .

假定运动为正压，在西南季风盛行期间，讨论了南海北部陆坡海域的地形Rossby波的非线性相互作用。

Under the condition of assuming that motion is barotropic during the south west monsoon wind prevailing , nonlinear interaction of topographic Rossby waves in the slope of the northern part of South China Sea is discussed in the present paper .