季风带
- 网络monsoon belt
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赤道印度洋沿着非洲东海岸,SST的季节变化受季风带影响显著,但在赤道中东印度洋,SST的季节循环特征不明显。
While the seasonal cycle of equatorial western Indian ocean is strongly affected by the monsoon , the seasonal variation of middle and eastern equatorial Indian Ocean is not apparent .
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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 .
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季风梅雨带水汽输送与动力强迫源结构
Water Vapor Transport and Dynamic Forcing Sources Structure over Meiyu Belt
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中国季风边缘带自然灾害的区域特征
Regional characters of natural disaster in marginal monsoon belt of China
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中国季风边缘带的自然灾害及成因
Natural disasters and their formation causes on Chinese monsoon marginal belt
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东亚季风边缘带上的植被变化
Vegetation variations along the monsoon boundary zone in East Asia
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季风汇合带与淮河流域的大暴雨
Relationship between monsoon confluent zone and very heavy rain over Huaihe River
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本文提出并讨论了季风边缘带的概念范围,并按大气圈、岩石圈和生物圈等三个方面对自然灾害的特点和成因进行了论证。
This paper discussed the concept and range of the monsoon marginal belt and demonstrated it from three aspects , that is aerosphere , lithosphere and biosphere .
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本文介绍了关于东亚大尺度低空急流背景流场的研究,指出其上游的季风西风带对它的重要作用,以及它与东非地区越赤道气流之间的关系。
A review regarding the investigation of the background circulation of large scale low-level jet over East Asia is given , which indicates the important effect of the monsoon westerlies on LLJ and the relationship between LLJ and cross-equatorial currents .
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东亚季风边缘活动带研究综述
Research on East Asian Summer Monsoon : A Review
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地处内陆非季风区干旱带的天山,是新疆地区风成黄土的重要分布区之一。
The Tianshan Mountains which located in non-monsoon region , is one of important distribution areas of eolian loess in the Xinjiang region .
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研究发现:冬季南海被东北季风最大风速带的轴线分成两部分,南海深水海盆东南部正的风应力旋度驱动一个气旋式环流。
The winter SCS is divided into two parts by the axis of the maximum northeasterly monsoonal winds . The positive wind curl in the southeastern half of the ocean drives a cyclonic gyre circulation in the deep basin .
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这种高纬度北大西洋气候与中低纬度的亚洲季风之间通过西风带的紧密结合,构成了北半球太阳-海洋-大气之间偶合的气候体系。
This type of the tie linkage between Northern Atlantic climate in higher latitude and Asian summer monsoon in middle-low by westerly wind zone consists of the coupled climate system between Sun-ocean-atmosphere in Northern Hemisphere . 3 .
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西风带作为北大西洋气候区和东亚季风气候区之间的联系纽带,对东亚季风气候和西风带气候具有重要影响,西风带在一定意义上控制着东亚季风的北界。
Westerly wind as a link between the climates of the North Atlantic and East Asian monsoon area , has great effect on the climates of East Asian monsoon area and westerly wind area .
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结果表明,模式成功模拟出对流层低层的季风系统,包括经典的热季风以及副热带季风和温寒带季风。
The result indicates that the model successfully simulates the monsoon system in the lower troposphere including the classic tropical monsoon , the subtropical monsoon and the temperate-frigid monsoon .