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.
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.
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.
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.
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.
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.
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.
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.
利用GCM（大气环流模式）完成的一系列改变青藏高原地形高度的数值试验说明，东亚季风气候变化非常敏感地响应于高原隆升。
Simulations of climate variables from General Circulation Models(GCMs)usually contain large deviation due to the low resolution, which makes it difficult for regional studies.
利用GCM（大气环流模式）完成的一系列改变青藏高原地形高度的数值试验说明，东亚季风气候变化非常敏感地响应于高原隆升。
Simulations of climate variables from General Circulation Models(GCMs)usually contain large deviation due to the low resolution, which makes it difficult for regional studies.
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