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The results suggest that: 1 This process is generated because northward inverted trough of typhoon Haitang combines with weak cold air in westerly belt, which is a classical reciprocity process between mid and low latitude weather systems.

结果表明:(1)台风北伸倒槽与西风带弱冷空气结合造成了这次大暴雨过程,是典型的中低纬系统相互作用过程。

As one of the aridest regions in Asia, Qaidam Basin is located in the center of Euroasia mainland. The region is very sensitive to global change owing to its location at the boundary between the middle latitude West wind system and the East Asia monsoon system.

柴达木盆地地处亚欧大陆腹地,是亚洲大陆干极核心,处於中纬西风带和东亚季风系统的交界带,对气候变化极为敏感。

The impact of the vertical shear on intensity variation of tropical cyclones at 12 hours before is the greatest.

Riehl等[6]提出,在低层东风带和上层西风带间的强垂直切变会阻止TC的发展加强

The results show that for the global scale characteristics of the vertically integrated vapor flux fields, which is described in terms of the rotational and divergent components of the stationary parts of the vapor field, both GOALS and FGCM--0 can reproduce the subtropical gyres in each hemisphere, the eastward water va- por transport of the mid--latitude westerlies, and the westward vapor transport of equatorial easterlies reasonably, though the precise positions of the gyres simulated by GOALS, and the intensities of the gyre centers in FGCM--0 do not match the observations accurately.

结果表明:(1)对垂直积分的水汽通量场的流函数及其对应的无辐散水汽通量矢量的模拟,三个耦合模式都能够较为合理地再现副热带大洋的涡旋结构、中纬度西风带的东向水汽输送、赤道东风带的西向水汽输送和东亚夏季风水汽输送等行星尺度特征及其季节变化,只是GOALS的涡旋位置、FGCM-0的涡旋中心强度,较之实际略有偏差。

By using the NCEP/NCAR (National Center for Environmental Prediction/National Center for Atmospheric Research) reanalysis of daily with the horizontal resolution of 10°×10°(lat./lon. grid), the representative Pacific area (0°~ 60°N, 160°E~120°W) in northern hemisphere summer is chosen to analyse the 3D wind field, according to which the mean meridional circulation of the lower and middle latitudes, especially the Ferrel cell, is studied and a new concept model of Ferrel cell is carried out. Compared with the classical model, the new one describes more precisely the low and high level winds and has the ability to describe how the westerlies sustain on the real rotating Earth.

本文利用1998~2003年的NCEP/NCAR(National Center for Environmental Prediction/National Center for Atmospheric Research,美国国家环境预报中心/美国国家大气研究中心)再分析资料(10°×10°,经/纬度网格),根据北半球夏季(6~8月)太平洋地区(0°~60°N;160°E~120°W)的三维风场的基本特征,分析了北半球夏季太平洋地区平均经圈环流,特别是Ferrel环流的特征,发现Ferrel环流具有与已往研究不同的性质,并在此基础上提出了Ferrel环流新的概念模型,与过去的经典的环流概念模型相比能较好地描述高低空环流的基本特征,同时在考虑地球自转效应下,能够完满地解释中高纬度西风带的维持。

By using the NCEP/NCAR (National Center for Environmental Prediction/National Center for Atmospheric Research) reanalysis of daily with the horizontal resolution of 1.0°x1.0°(lat./lon. grid), the representative Pacific area (0°~60°N, 160°E~120°W) in northern hemisphere summer (Jun-Jul-Aug) is chosen to analyse the 3-D wind field, according to which the mean meridional circulation of the lower and middle latitudes, especially the Ferrel cell, is studied and a new concept model of Ferrel cell is carried out. Compared with the classical model, the new one describes more precisely the low- and high- level winds and has the ability to describe how the westerlies sustain on the real rotating Earth.

本文利用1998~2003年的NCEP/NCARNational Center for Environmental Prediction/National Center for Atmospheric Research,美国国家环境预报中心/美国国家大气研究中心)再分析资料(1.0°×l.0°,经/纬度网格),根据北半球夏季(6~8月)太平洋地区(0°~60°N; 160°E~120°W的三维风场的基本特征,分析了北半球夏季太平洋地区平均经圈环流,特别是Ferrel环流的特征,发现Ferrel环流具有与已往研究不同的性质,并在此基础上提出了Ferrel环流新的概念模型,与过去的经典的环流概念模型相比能较好地描述高低空环流的基本特征,同时在考虑地球自转效应下,能够完满地解释中高纬度西风带的维持。

Rammasun started to weaken on 11 May. It moved into the westerlies on 12 May and turned to move north-northeastwards.

威马逊於5月11日逐渐减弱,翌日移入西风带及转向东北移动。

Wang Yang first to the North Pole, but here it seems that all are familiar with, particularly over land where the white world. In 1998, she was aboard the icebreaker across the former Soviet Union "devil westerly wind belt," visited the Antarctic.

王秋杨第一次到北极来,却对这里的一切似乎都很熟悉,尤其是那片严寒笼罩的白色天地。1998年,她曾经乘坐前苏联的破冰船穿越&魔鬼西风带&到过南极。

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。

The changes of monthly mean wind speed and monthly mean temperature with time have different laws between desert hinterlands and its fringe.

初步得到了以下一些结论:(1)塔里木盆地的环流形势是在高空西风带的背景下,经过青藏高原、天山山脉的动力分支和抬升,以及沙漠本身的热力作用下共同形成的。

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