The orographic influence on the winter monsoon is greater than that on the summer one.
高原隆升对东亚冬季风的影响远大于对夏季风的影响。
This kind of anomalous atmospheric temperature variability is mainly influenced by the winter monsoon.
这种气温的异常变化主要受东亚冬季风的直接影响。
Studies of the winter monsoon evolution can help us to understand the dynamic mechanism to climate change in the east-Asian areas.
研究冬季风演化历史将有助于深入理解全球变化背景下，东亚地区气候变化的动力机制。
In China, the winter monsoon brings dust storms.
在中国，冬天的季风带来沙尘暴。
Therefore, East Asian winter monsoon is a precursory signal for the prediction of disastrous climate anomalies.
因此，东亚冬季风是一种预测短期灾害性气候异常的前兆信号。
The East Asian winter monsoon anomaly has biseasonal effect on the circulation and weather in the following summer.
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。
We point out that the intensity of Indian winter monsoon is just a key symptom to mirror the tectonics of the plateau.
文章还提出印度冬季季风强度是反映高原构造活动关键标志的观点。
In the whole Last glacial, the winter monsoon was much powerful, even in MIS3 stage, the climate was still dry and cold.
整个末次冰期，研究区的冬季风较强盛，即使在MIS3阶段，气候也以干冷为主。
The relationship of autumn Kuroshio region SSTA with the East Asian winter monsoon and Chinese winter climate is analyzed.
分析了秋季黑潮区域海表温度异常与东亚冬季风以及我国冬季气候的关系。
Summer monsoon was weaker and winter monsoon stronger. Precipitation decreased, and eolian dust deposition was accelerated.
这一时期夏季风减弱，冬季风增强，风成黄土堆积，降水减少。
Results show that there is a closely relation between the autumn Kuroshio region SSTA and the East Asian winter monsoon index.
结果表明：秋季黑潮区域海温与东亚冬季风指数有明显的正相关关系。
The main results are as follows: the influence of anomalous winter monsoon on the wind field in SCS region may persist from winter to summer.
结果表明，冬季风异常对流场的影响可以从冬季持续至春、夏季。
Zhu Yanfeng. 2008. An index of East Asian winter monsoon applied to description the Chinese mainland winter temperature changes[J]. Acta Meteor Sinica, 66(5):781-788.
朱艳峰.2008。一个适用于描述中国大陆冬季气温变化的东亚冬季风指数[J]。气象学报，66（5）：781-788。
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.
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。
Correlationanalysis method is used to investigate the impact of the East-Asian winter monsoon and summer monsoon impact on the temperature and precipitation of Northwest China.
运用相关分析方法研究了东亚冬、夏季风对中国西北地区气温和降水的影响。结果表明，东亚季风对西北地区干旱形成的影响是显著的。
It is suggested that the monsoon abnormity in plateau is affected by the special surface thermotics which is the media of winter monsoon abnormity leading to summer monsoon abnormity.
高原季风异常可能与高原下垫面热力异常有关，从而推测冬季风异常通过高原这个巨大的热载体而影响夏季风异常。
The East Asian summer and winter monsoon intensity indices are constructed by using the SLP data for the period of 1873~1996/1997 and their interannual and inter decadal variabilities are analyzed.
用1873～1996／1997年资料，延长计算了东亚冬夏季风强度指数，研究了指数的年际及年代际变化的主要特征。
The East Asian summer and winter monsoon intensity indices are constructed by using the SLP data for the period of 1873~1996/1997 and their interannual and inter decadal variabilities are analyzed.
用1873～1996／1997年资料，延长计算了东亚冬夏季风强度指数，研究了指数的年际及年代际变化的主要特征。
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