monsoon的例句大全

A Study of the Indian Ocean Dipole Influence on Climate Variations over East Asian Monsoon Region

印度洋偶极子对东亚季风区天气气候的影响

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The relation between the number of the May heavy storm days in Yunnan and the Asia monsoon intensity index is studied by correlation analysis and EOF methods.

利用相关分析和EOF方法，研究了云南5月大雨、暴雨日数与亚洲季风这一大尺度气候环流背景变化的关系。

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The results show: ( 1) The temperature had obvious climate characteristics of land monsoon and normal distribution;

结果表明：（1）枣庄气温具有明显的季风性大陆气候特征，总体呈现正态分布。

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Meanwhile, vegetation can also reduce the sea-land temperature contrast and weaken the Asian summer monsoon.

同时，植被的存在使大陆潜热释放增强，气温下降，减小了海陆温度对比，亚洲夏季风也有所减弱。

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A three-dimensional planetary convective cell is proposed to interpret the global abnormal monsoon circulation, based on the surface temperature contrast between the middle Equatorial Pacific and the Western Pacific ( or the Eastern Asia).

在赤道中太平洋和西太平洋（或东亚）之间表面温度对比的基础上，提出了三维行星对流环流，并以此来解释异常的季风环流。

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The results of this study would undoubtedly be useful for applying the stable isotopes as a temperature indicator in some research fields such as glaciology, hydrology and palaeoclimatology in the monsoon-affected areas of China.

本结果有助于将稳定同位素温度指示剂正确地应用于我国季风气候区的冰川学、水文学以及古气候学等研究领域。

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According to the basic characteristic of activities of South China Sea summer monsoon, an index of South China Sea summer monsoon intensity, Is, which is composed by both dynamic factor ( southwest wind component) and thermodynamic factor ( OLR) was studied in this paper.

依据南海夏季风活动的基本特征，设计了一个动力学因子（西南风分量）与热力学因子（OLR）相结合标准化的南海夏季风强度指数Is。

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The effects of three dimensional structure of heating field on the summer monsoon circulation in Asia

加热场的三维结构对亚洲夏季风环流的影响

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Therefore, it seems that the onset of South China Sea summer monsoon can be predicted with the heat content of the western Pacific Ocean warm pool, the key for which is to find a station representing the warm pool in terms of heat content.

据此，我们可以通过西太平洋暖池热含量的变化来预测南海夏季风的爆发。

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Composite Study of the Surface Thermal Anomaly over the East Asia in Strong and Weak SCS Summer Monsoon Years

南海夏季风强弱年东亚地表热力异常特征的合成研究

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Interannual and Interdecadal Varieties of Summer Rain-belt s Propagation and Corresponding Characters of Height and Sea Temperature; ACTIVITY CHARACTERISTICS OF EAST ASIA SUMMER MONSOON AND RAINFALL DISTRIBUTION OVER EASTERN CHINA IN 2006

中国夏季雨带推进过程的年际年代际变化及其相关海气背景分析2006年东亚夏季风活动特征与我国东部雨带分布

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Land-air heat exchange and thermal boundary layer structure before and after the establishment of South China Sea Monsoon over Pearl River Delta

南海季风建立前后珠江三角洲的陆气热量交换与热力边界层结构特征

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The land-sea pressure difference and thermal difference decrease, resulting in the weakening of monsoon;

海陆气压差和海陆温差的减小导致季风减弱；

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Like the East Asia Monsoon, the Southern Asia Monsoon is also also caused by Thermal difference between sea and land.

亚洲南部的季风（下称南亚季风）和亚洲东部的季风（下称东亚季风）一样，都属于海陆季风，主要是由海陆之间的热力差异引起的。

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The seasonal movement of planetary wind system only enhances the formation of the Southern Asia Monsoon, and its effective strenth is conditioned by thermal difference between sea and Land.

行星风带的季节移动对南亚地区的影响强度受到海陆热力差异的制约，其固有的季节移动作用，对南亚季风形成只起加强的作用。

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A contrastive analysis of two indexes of the east Asian monsoon reveals that there is a relation between the index of sea-land thermal difference and the summer rainfall in Shandong Province.

对2种东亚夏季风指数进行了对比分析，选择1种能较好地表征山东夏季降水的夏季风指数。

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The index reflect the variations of both the thermal low pressure centering in Mongolia and the subtropical high in the western Pacific very well and also indicate an intensity of summer monsoon in the East Asian subtropics and an anomaly of rainfall along the valleys of the Yangtze River.

该指数不仅能够较好地反映以蒙古为中心的东亚大陆热低压和西太平洋副热带高压的变化特征，还能够指示东亚副热带夏季风的强弱以及中国长江流域降水的异常变化。

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Results show that the summer monsoon bears significant anti correlation relationship with the anti Walker circulation over Indian and western Pacific oceans and the cross equatorial monsoon circulation in Asia.

分析表明：东亚夏季风年际变化与印度洋-西太平洋上空反Walker环流及夏季越赤道南北半球间的季风环流呈显著正相关关系。

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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.

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。

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Climate and monsoon features of the Indian Ocean north of 35 ° s

35°S以北的印度洋的气候状况和季风特征

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