季风环流可以分解为经向环流和纬向环流。
The monsoon circulation can be decomposed into the zonal circulation and the meridional circulation.
黄士松，汤明敏。我国南方初夏汛期和东亚季风环流。热带气象学报。
Huang shisong tang mingmin. the early summer flood periods of southern china and the summer monsoon circulation of east asia. journal of tropical meteorolog.
珠穆朗玛峰东侧东绒布冰川积累区的降水主要是由印度夏季风环流带来的。
The precipitation in the accumulation zone of the East Rongbuk Glacier on the east slope of the Mount Qomolangma is mostly brought on by Indian summer monsoon.
ENSO事件对亚洲季风有很大影响，特别是对东亚夏季风环流有较大影响。
ENSO event has a large influence on Asian monsoon, particularly on the East Asian monsoon.
试验结果表明，热带海洋的热状况是影响亚洲季风环流和降水的一个重要因素。
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.
印度夏季风环流建立时间较晚，它与索马里低空急流，北支高空东风急流相联系。
The summer monsoon circulation in India was established somewhat later, accompanying with the Somali low jer and the northern upper Easterlies.
红粘土的粒度分布表明，东亚冬季风环流而非北半球西风环流控制着红粘土物质的堆积过程。
The size distribution of red clay showed that the accumulation of red clay was controlled by East Asian monsoon circulation rather than westerly circulation.
东亚季风环流对华北降水和气温的共同作用，导致华北地区降水蒸发差发生年际和年代际变化。
The conjunctive actions of the atmosphere circulation over East Asia area on the precipitation and air temperature induced the interannual and interdecadal variations of the DPE in the North China.
利用NCEP再分析的1982～ 1996年的风场和高度场资料，分析讨论了亚洲热带夏季风环流的若干基本特征；
NCEP reanalysis dataset of 1982~1996 is used to analyze the basic features of the Asian Summer monsoon circulation.
采用NCEP/NCAR再分析资料和NCAR海温资料，对ENSO循环不同阶段东亚夏季风环流的变化进行了分析。
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.
指出与低纬深厚积云对流相联的凝结加热对亚洲夏季风环流所起的重要作用和大气定常行星波响应对加热场的垂直结构的敏感性。
It is shown that the aloft heating connected with latent heating, especially the deep condensation heating associated with cumulus convection in low latitudes, plays a crucial part for the Asian…
利用ECMWF高度场资料，详细分析了1985年（旱年）和1991年（涝年）5月主要季风环流系统的旬平均和旬距平特征。
In the context of ECMWF height data, investigation is conducted of the decadal mean and anomaly characteristics of major summer monsoon systems in May, 1985 (of drought) and 1991 (severe flood).
融冰将阻断北大西洋环流，将改变全球天气模式，最终关闭亚洲季风季节。
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.
平流层和对流层环流的相互作用及其与季风建立的关系很值得进一步研究。
The interactions between stratospheric and the tropospheric circulations and their relation to the onset of monsoons need further investigation.
结果陕北地区土地沙漠化及水土流失受全球气候变化、青藏高原抬升、西风环流变化、东亚季风演化的控制；
Results The land desertification in north of Shaanxi is controlled by the Tibet Plateau uplift, the changes of west wind circulation and east-Asian monsoon evolution.
穿越赤道区的季风和信风的环流格局，致使新第三纪和第四纪中国与澳大利亚的气候系统的相关性更强。
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.
穿越赤道区的季风和信风的环流格局致使晚第三纪和第四纪中国与澳大利亚的气候系统的相关性更强。
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.
季风强弱与冬夏大气环流差异是决定云南气象灾害的主要气候背景。
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.
东亚冬季风异常可隔季影响到我国次年夏季环流和天气状况的异常。
The East Asian winter monsoon anomaly has biseasonal effect on the circulation and weather in the following summer.
潜热输送与我国环流特征及季风进退有密切的关系。
The latent heat transfer in China is closely related to the characteristics of circulation and the advance and retreat of monsoon winds.
在异常的冬季风偏北风分量强迫下，西太平洋上形成的偏差气旋环流在夏季已不存在，这时东亚夏季风反而增强。
The northerly component of the winter monsoon anomaly makes the anomalous cyclone over the western Pacific not exist and the East Asian summer monsoon becomes stronger.
喜马拉雅山区毗邻南亚季风区，其陡峭的地形和复杂的地表状态在强烈太阳辐射条件下形成了特殊的局地环流系统。
The Himalayas is near the South Asian monsoon region, with a special local circulation system induced by its steep topography and complex terrains.
结果表明：印度洋海温偶极振荡异常，引起了大气环流的异常，影响了季风强度和雨带分布。
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.
利用1982 ~ 1996年每天两次的NCEP再分析资料，研究青藏高原地面加热场的日变化对亚洲季风区环流的影响。
The impact of the diurnal variation of the surface heating in the Tibetan Plateau on the circulation over the Asian monsoon region is analyzed using the twice daily NCEP data from 1982 to 1996.
影响该流域夏季降水的环流系统为西风带阻塞形势下的低值系统和东亚夏季风。
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.
而亚洲热带大气环流的年际变化与华南春季风降水的变化关系不大。
Changes in the Asian tropical atmospheric circulation has little influence on the spring monsoon in South China according to this research.
绝大多数年份季风建立时有环流突变发生，但也有少数年份呈调和变化或二次突变。
The onset of summer monsoon in South China Sea region is characterized by the abrupt change of flow field in most years, but a few years characterized by harmonic change(no abrupt transition).
季风是全球气候系统中一种重要的大气环流系统，随着气候学研究及季风动力学研究的深入，国内外学者对季风的形成及其变率问题的研究取得了很大进展。
With the deepening of study on climate and monsoon dynamics, great advances in the research on the mechanism and variability are achieved by scholars in China and other countries.
但对局部区域而言，可以发现在季风爆发前后其环流结构有明显的差异。
For some local areas, there existed some apparent differences in the circulation structures around the monsoon onset.
通过利用一个分区性的正压、斜压衔接模式，重点考察了南海环流对于以不同方式变化的季风转变时的响应。
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.
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