• It distincts four seasons and moderate climate due to the influence from monsoon circulation.

    亚热带湿润气候区,四季分明,气候温和

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  • The monsoon circulation can be decomposed into the zonal circulation and the meridional circulation.

    季风环流可以分解为经环流向环流。

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  • NCEP reanalysis dataset of 1982~1996 is used to analyze the basic features of the Asian Summer monsoon circulation.

    利用NCEP分析1982~ 1996年风场和高度场资料,分析讨论了亚洲热带夏季环流的若干基本特征

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  • The summer monsoon circulation in India was established somewhat later, accompanying with the Somali low jer and the northern upper Easterlies.

    印度夏季环流建立时间较,它索马里低空急流高空东风急流相联系。

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  • The size distribution of red clay showed that the accumulation of red clay was controlled by East Asian monsoon circulation rather than westerly circulation.

    粘土粒度分布表明东亚冬季风环流非北半球西风环流控制着红粘土物质堆积过程。

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  • Huang shisong tang mingmin. the early summer flood periods of southern china and the summer monsoon circulation of east asia. journal of tropical meteorolog.

    黄士松,汤明敏。我国南方初夏汛期东亚季风环流热带气象学报

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  • The result shows that the thermal condition of the tropical seas is an important factor in affecting the variability of the Asian monsoon circulation and precipitation.

    试验结果表明热带海洋状况影响亚洲季风环流降水一个重要因素

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  • The sea surface temperature (SST) over equatorial eastern Pacific was the most important force factor for the seasonal and annual variation of east Asian monsoon circulation.

    冬季赤道太平洋海温变化冬、夏东亚环流季节以及年际变化重要强迫因子

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  • Meanwhile, the anomaly of the atmospheric circulation over the high latitude Eurasia during spring is crucial to the summer monsoon circulation and precipitation over East Asia.

    欧亚高纬大气环流春季异常对东亚区夏季大气环流降水异常起着非常重要的作用。

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  • The variation of East Asia summer monsoon circulation in different periods of ENSO cycle has been analyzed by using meteorological data from NCEP/NCAR and sea surface temperature data from NCAR.

    采用NCEP/NCAR分析资料和NCAR海温资料,对ENSO循环不同阶段东亚夏季环流变化进行了分析。

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  • Because the Arabian Sea is landlocked to the north, it is less influenced by large-scale ocean circulation and more strongly influenced by the monsoon winds.

    由于阿拉伯北面陆封,所以大规模洋流对此处作用不大,而季风可以大显身手。

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  • And that melting ice could interrupt the north Atlantic ocean circulation, which would alter global weather patterns and ultimately switch off the Asian monsoon season.

    阻断北大西洋环流改变全球天气模式最终关闭亚洲季风季节。

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  • In the Late Tertiary and Quaternary the climate systems of China and Australia have become increasingly linked due to the monsoon and trade wind circulation patterns across the equatorial region.

    穿越赤道区的季风信风环流格局,致使新第三纪第四纪中国澳大利亚气候系统相关性更强。

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  • In the Late Teniary and Quatemary the climate systems of China and Australia have become increasingly linked due to the monsoon and trade wind circulation patterns across the equatorial region.

    穿越赤道区的季风信风环流格局致使第三纪第四纪中国澳大利亚气候系统的相关性更强。

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  • Results show that the IOD anomaly results in anomalous atmospheric circulation, which affects the distribution of the rain belt during rainy seasons in China and the East Asian monsoon.

    结果表明印度洋海温偶极振荡异常,引起了大气环流异常,影响季风强度雨带分布

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  • The East Asian winter monsoon anomaly has biseasonal effect on the circulation and weather in the following summer.

    东亚冬季异常可隔影响到我国次年夏季环流天气状况的异常。

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  • The circulation cells which affect summer precipitation are a low system on the blocking trend of the westerly belt and the summer monsoon of East -Asia.

    影响流域夏季降水环流系统西风带阻塞形势下低值系统东亚夏季

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  • Changes in the Asian tropical atmospheric circulation has little influence on the spring monsoon in South China according to this research.

    亚洲热带大气环流的年际变化华南春季风降水变化关系不大

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  • The Himalayas is near the South Asian monsoon region, with a special local circulation system induced by its steep topography and complex terrains.

    喜马拉雅山区毗邻南亚季风区陡峭地形复杂的地表状态强烈太阳辐射条件下形成了特殊局地环流系统

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  • For some local areas, there existed some apparent differences in the circulation structures around the monsoon onset.

    局部区域而言,可以发现季风爆发前后环流结构明显差异

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  • A divisional barotropic and baroclinic connection model is employed, emphasizing on studying the response of the South China Sea (SCS) circulation to the transition of monsoon in different ways.

    通过利用一个分区斜压衔接模式重点考察南海环流对于以不同方式变化季风转变时的响应

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  • The strong or weak monsoon activities and the difference of general atmospheric circulation in winter and summer over Yunnan are the climatic background to form weather disasters.

    季风强弱大气环流差异决定云南气象灾害主要气候背景

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  • The latent heat transfer in China is closely related to the characteristics of circulation and the advance and retreat of monsoon winds.

    潜热输送我国环流特征季风进退密切关系。

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  • The Australian high as an important circulation member of the East Asian summer monsoon system has significant impacts on the summertime climate of China.

    澳大利亚高压东亚夏季系统重要成员之一中国夏季气候存在显著影响

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  • The circulation cell is very clear on the average map of monsoon period. It's meridional scale is about 1500km with a top up to 100 hPa .

    这个环流梅雨期间平均图上表现十分清楚南北范围1500公里顶部可达100百,中心约在距地7—9公里之间。

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  • The circulation cell is very clear on the average map of monsoon period. It's meridional scale is about 1500km with a top up to 100 hPa .

    这个环流梅雨期间平均图上表现十分清楚南北范围1500公里顶部可达100百,中心约在距地7—9公里之间。

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