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The pentad right after the last pentad with the SCS summer monsoon covering 40% or more of the above area is defined as the ending time of the SCS summer monsoon.

定义某年某侯南海夏季风面积最后一次超过百分之四十后一侯为南海夏季风的结束日期。

During the four years study on the project, we develop a dynamical forecast model that describing the subtropical ridge surface. A new theory on the role of the land-sea thermal difference on the formation of the Subtropical High is advanced. It is concluded that in the summer subtropics over each continent and its adjacent ocean LO, SE, CO, and a double-dominant heating from west to east compose a LOSECOD heating quadruplet. The influence of the Eurasia continent on SH varies according to the seasonal variation. From the ideal numerical simulation it is shown the important role of the Eaiuan continent and the huge topography on the mechanism of formation and mantanence of the SH during the summer. It is verified by the numerical simulation that the extension of the subtropical continent into the tropics greatly enhances the " East Asian monsoon". Through the Rossby energy dissipation theory it is verified that the deep latent convective heating induces the onset of the South China Sea monsoon over the Bay of Bengal. The relationship and mechanism between the precipitaiton over the East Asia and the Subtropicla high is illustrated by the data. It is also found the close phase lock between the east-west shift of the SH and the disturbence of the east wind belt over the tropical troposphere. The interaction between the structure and activity feature of the SH and the Meiyu over the Yangtze-Huaihe river valley is revealed from the data. The numerical simulation verified the impact of the different SH pattern on the path of the typhoon.

本项目的研究发展了描述副热带高压脊面变化的动力模型,提出了夏季副热带地区四叶型非绝热加热分布型及相应环流拼图的创新理论;明确了大陆尺度的海陆热力差异在副热带高压形成中的作用;指出欧亚地形对副热带高压和气候的影响随季节变化而变化,通过数值试验证明春季青藏高原的感热加热对亚洲夏季风的爆发地点起了"锚定"的作用,进一步证实了副热带高压断裂和亚洲夏季风的最早爆发地点发生在孟加拉湾东岸;利用Rossby波能量频散理论证明了孟加拉湾深对流潜热释放诱导南海季风爆发的机制;揭示了东亚季风降水的季节内变化与西太副高的关系及机理;揭示了西太副高与东西风带中扰动之间的相互作用过程,指出西太副高的东西活动与热带对流层上空东风带扰动和中纬度西风带扰动的移动和锁相密切相关;研究了夏季淮河流域梅雨期间副高结构和活动特征及其与江淮暴雨的相互作用;验证了不同副热带高压形态对台风路径的不同影响;通过数值试验证明了欧亚大陆和青藏高原等大地形对副热带高压形成和维持的重要作用。

Precipitation in Heilongjiang Province of China increased slightly from 1960 to 2000. Adopting the method proposed by Arthur N. Samel, we separated monsoon rainband rain and calculated the initial and final date of monsoon rainband of each year and each station.

为了分析黑龙江省夏季季风的变化规律和夏季季风与年降水之间关系的变化,采用Samel发明的方法,用逐日降雨量数据计算每一年夏季季风到达、离开、停留在黑龙江省的时间。

After the monsoon onset, the southwesterly monsoon transported the volume of warm and wet air to the SCS and the convection enhanced. So, the stratification was unstable and precipitation was also falling.

这主要是由于季风爆发后,西南季风把大量暖湿空气输送到南海地区,对流活动增强,大气呈现不稳定层结并伴有降水发生的结果。

The analysis of proxy indices of winter and summer monsoon indicated that East Asia Monsoon is characterized by periodical evolution and vibratility during Late Cenozoic.

四、根据对冬、夏季风气候代用指标的时间序列分析表明,晚新生代东亚古季风具有阶段性演化和在冰期—间冰期尺度上的波动特征。

The APW in summer is less than 25 mm which is the least limit value of monsoon areas.This means that Xinjiang is not affected by monsoon.The geographic distribution of APW is adverse with that of precipitation,videlicet,higherAPW values corresponding to lower precipitation values.With the effects of westerly winds,the APW mode presents as an uniform change within Xinjiang area and has a stable distribution.It is very different from Xinjiang rainfall mode which changes a lot spatially.As mentioned above,there is no obvious change during 1961~2000,this indicates that APW is not a dominant factor determining precipitation,it is the result of dynamic condition,water vapor convergence and other causes.

APW的地理分布与实际降水量分布相反,其最大区域却为降水量最小区,受西风带影响,新疆APW模态主要表现全疆一致变化,分布稳定,与降水模态分布差异性大有显著不同,且近40年来无显著变化趋势,表明决定新疆降水差异的根本原因不在于水汽的多少,而是由降水产生的动力条件、水汽辐合和其它因素差异决定的。

Shenyang's climate is a monsoon-influenced humid continental climate (Koppen climate classification Dwa) characterized by hot, humid summers, due to the monsoon, and dry, cold winters, due to the Siberian anticyclone.

沉阳的气候是一个季风影响的湿润大陆性气候的特点是高温,高湿的夏季,由于季风和干旱,寒冷的冬季,由于西伯利亚高气压。

The results reveal that:a Pentadactyl vapor transportation in East-Asia change with the appearing , strengthening , weakening , and disappearing of the South China Sea monsoon, the Indian monsoon, subtropical high etc..b Southerly vapor transportation of each longitude areas in East-Asia have different characters in appearance time , speed to north , the place of north bound , speed to south , etc..

主要得出以下结论:(1)东亚地区各候各区域水汽输送的变化,伴随着南海季风、印度季风、副高等天气事件或系统的发生、加强、减弱和消失。(2)各个经度带的偏南风水汽输送在出现时间、北抬进程速度、北界位置、南撤速度等方面均体现了不同的特征;西太平洋副高边缘的东南风水汽输送具有迂回西扩和快速东撤的特点,并且在强盛期能够影响到我国西北地区。

The monsoon rains, which feed India's unirrigated farmland, have been fickle, inflicting drought on almost half of India's districts, followed by floods in some areas as the monsoon departed.

哺育印度干旱农田的季风雨反复无常,使一半以上的印度地区遭受旱灾的折磨,接着便是季风过后在一些地区发生的涝灾。

Based on NCEP/NCAR reanalysis data, the structure and variation of Tropical Easterly Jet and its relationship with the distribution of rainfall in Asia and Africa are analyzed. In addition, the Asian summer monsoon indices are reappraised and the secular variation of monsoon is studied.

本文主要是用NCEP/NCAR再分析资料研究了热带东风急流的结构,多尺度变化特征及其与亚非季风降水的关系,并且在此基础上重新评估亚洲夏季风指数及研究季风的长期变化,最后比较了NCEP/NCAR与ERA-40再分析资料的差异。

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