Monsoon, referring to the winter winds and summer monsoon impact.
季风，指冬季风和夏季风的影响。
The activity of summer monsoon may be another key climate signal in East Asia.
在东亚，夏季风的活动可能是另一个关键气候信号。
The previously winter Kuroshio SSTA relates greatly to the East Asian summer monsoon (EASM).
前期冬季黑潮区域海温异常与东亚夏季风存在显著的联系。
The numerical modeling of wind current is studied under winter and summer monsoon conditions.
本文对台湾海峡风海流的研究分为冬季和夏季两种情况来模拟。
Local people speak of the inevitable summer monsoon, which will bring relief from the spring drought.
夏季季风，这即将如期而至的“春旱救星”，随之也成为当地人谈论的话题。
When summer monsoon intensity is weak (strong), drought (flood) frequently happen in the North China Plane.
夏季风偏强(弱)年份，华北平原多发生雨涝(干旱)。
There is a considerable connection between ENSO and the interannual variations(QBO)of summer monsoon rainfall.
ENSO与东亚夏季风降水的年际变化以及准二年周期有着明显的联系。
Gentler but more persistent bad weather - the downpours of the summer monsoon - is also being taken into account.
缓和但持续的坏天气-夏季雨季的倾盆大雨-也被考虑。
NCEP reanalysis dataset of 1982~1996 is used to analyze the basic features of the Asian Summer monsoon circulation.
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；
The variations of the water vapor transportation paths is related with the weaken of summer monsoon over East Asia.
水汽输送通量和水汽输送轨迹的变化主要和东亚夏季风的逐渐减弱有关。
Results show that the existence and geometric shape of land-sea distribution crucially affect the Asian summer monsoon.
试验结果显示：海陆分布的存在以及海陆分布的几何形状对亚洲夏季风的形成有非常重要的影响。
Based on the method of composite analysis, the onset process of summer monsoon over South China Sea (SCS) is investigated.
采用合成分析方法研究了南海夏季风的爆发过程及其前期征兆。
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。
Most of India’s crucial rain is brought by the summer monsoon, which falls, with luck, in just a few weeks between June and September.
基本上印度最主要的降雨都是由夏季季风带来的。 即使在好的年节，这些雨水也只集中在六月和九月之间的一小段时间里。
In the Indian state of Punjab, farmers plant rice seedlings ahead of the summer monsoon rains, which are expected at the end of June.
在印度旁遮普邦，农民植物水稻幼苗，赶在预计在六月底的夏季气旋雨之前。
The summer monsoon reliably delivers an intense abundance of water, swelling rivers, lakes and flooding water-courses incredibly fast.
其次，夏季风带来的充沛降水，致使河流，湖泊以及洪水水道正在以惊人的速度迅速膨胀。
The influence of Northwest Pacific summer monsoon(NWPSM) characteristics and the structure of monsoon trough on typhoon genesis is studied.
研究了西北太平洋夏季风特征及其季风槽结构对台风生成的影响。
The summer monsoon was driven by global ice volume in the glacial-interglacial scale, and also driven by other factors in more little scale.
夏季风在冰期与间冰期尺度上受全球冰量的影响，但在更短时间尺度上有其它驱动因子。
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 statistical results show that the variation of summer rain belt pattern relates closely to the strength of summer monsoon in the East Asia.
分析表明：东亚夏季风强弱与我国夏季雨带类型之间有着一定的联系。
The results show that the summer monsoon of Nansha sea surface came from the west path and south path from the monsoon air current of this sea area.
结果表明：南沙海面夏季风来自南路和西路及本区的季风气流。
The Asian summer monsoon trough consists of two major components: the South China Sea (SCS) summer monsoon trough and the Indian summer monsoon trough.
亚洲夏季风槽包括两大重要组成部分，即南海夏季风槽和印度夏季风槽。
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。
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。我国南方初夏汛期和东亚季风环流。热带气象学报。
Two numerical experiments were performed by using ECMWF limited area model in order to assess the impact of radiative processes on the onset of summer monsoon.
应用ECMWF有限区域模式，设计了两个数值实验以估计辐射效应对于夏季风开始的影响。
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.
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。
In addition to natural variations in solar radiation, greenhouse gases such as carbon dioxide and aerosols such as soot can have an impact on the summer monsoon.
除了太阳辐射的自然变化之外，二氧化碳之类的温室气体和烟灰之类的气溶胶也可能对夏季季风有影响。
Results show that the Plateau summer monsoon, the summer temperature and precipitation in the upper reach of Changjiang river valley exist obvious change in phase.
结果表明，高原夏季风、长江上游夏季气温和降水均存在明显的阶段性变化特征。
Results show that the Plateau summer monsoon, the summer temperature and precipitation in the upper reach of Changjiang river valley exist obvious change in phase.
结果表明，高原夏季风、长江上游夏季气温和降水均存在明显的阶段性变化特征。
应用推荐