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The sensitivity experiment reveals that the SSTA of 1.5℃ can lead to anomalous neighborhood rainfall that extends northeastward and possibly reaches the south of China. Meanwhile, the anomaly of latent heat release due to rainfall stimulates a thermal adaptation of neighboring air and then causes the anomaly of SHWP.

敏感性试验结果表明,BOB1.5℃的海温异常可以引起邻近区域的降水异常响应,异常的降水向东北方向伸展,可以到华南;降水异常的凝结潜热释放造成了附近大气环流的热力适应,从而导致了西太副高的异常。

In this thesis, circulation of the West Pacific Ocean and the East China Sea is simulated, with a three dimensional baroclinic primitive equation model - MIT general circulation model.

本文采用麻省理工大学的环流模式MIT general circulation model,对西北太平洋和渤黄东海环流进行网格嵌套数值模拟,成功地得到了上述海区的环流特征和季节变化规律。

It is indicated that the updrafts of the Arabian Sea meridional cell tube and the south zonal cell tube arrive in the SCS at the same time in May, which brings strong convective precipitation. Meanwhile, the westerly of the meridional cell tube and the southerly of the south zonal cell tube combine together to form the southwesterly at the low levels, resulting in the onset of the SCS monsoon.

研究发现阿拉伯海经向环流管的上升气流和南半球纬向环流管的上升气流在5月份同时到达南海,经向环流管低层的偏西风和纬向环流管低层的偏南风共同组成西南风,于是5月份西南季风在南海地区首先爆发。

The thickness of the ice cover on the wall surface heat transfer is greater than the thickness of it on the air heat transfer form. The thickness of the ice cover on the wall surface heat transfer along the way changes slowly, but it on the air heat transfer along the way changes significantly. Reducing the entrance velocity, lowering the wall surface or air temperature, the formation of the thickness of the ice cover will increase; in the 3D circumstances, The thickness of the ice cover was relatively uniform in the import of the U-turn model, the ice cover was gradual accumulation in the convex bank when the stream traversed the import of the U-turn model, the thickness of the ice cover in the convex bank was significantly bigger than the thickness in the concave bank. The temperature field under the ice cover tends to be complex because of the existence of the secondary flows. The temperature in the convex bank is greater than it in the concave bank. Compared with the data from experiments, the laws in the numerical simulation are similar with them in the experiments

模拟结果显示:二维情况下,运用壁面传热形成的冰盖厚度大于运用空气传热形成的冰盖厚度,壁面传热形成的冰盖厚度沿程变化缓慢,而空气传热形成的冰盖厚度沿程变化明显,减小入口流速,降低壁面或空气温度等,形成冰盖的厚度都会增大;三维情况下,弯道入口处凸、凹岸形成的冰盖厚度基本相同,进入弯道后,凸岸形成的冰盖厚度逐渐增大,而凹岸的冰盖厚度逐渐减小,受横向环流的影响,冰盖下水流的温度场趋向复杂,并且凸岸的温度小于凹岸的温度;与实验室实验所得数据相比较,数值模拟研究得到的规律基本符合实验规律。

Based on the review of the description of subtropical high and the research on its formation, fluctuation characteristics and physical mechanisms, it is found that the subtropical high is refered to the area where pressure is relatively larger. Its formation is due to the existence of mean meridional circulation that accumulates air mass to subtropical areas. The subtropical high is belt-like with meridionally non-uniform feature and this is a zonal mean point of view.

通过对副高的描述、形成及演变特征和物理机理的研究进行回顾,认为:副高是相对的气压的高值,是由于平均经圈环流的存在,使得有空气质量在副热带地区的堆积而形成的,成为带状,表现出在经度方向的不均匀,这是一种纬向平均的观点;同时,在这个平均的高压带上常常有闭合的单体存在,表现出纬向的不均匀。

And the dull roar of blowers circulating air.

产生的噪音及促使空气环流的鼓风机发出的单调的轰鸣声

E. , approximately four months; 2 the active periods occur much longer than the non-active periods; the main climatic characteristics of the non-active periods, compared with the active periods, is weaker monsoon with westerlies at 850-hPa and easterlies at 200-hPa on the deviation fields of circulations over the SCS (active time minus non-active time); it is warmer in the active periods than in the non-active periods at lower and upper levels; 3 in most circumstances, the low frequency vibrations of the summer monsoon and its rainfall are quite in phase.

2其中活跃期出现时间要比非活跃期长的多。与活跃期相比非活跃期主要气候特征表现为季风的减弱,在环流的偏差场上在南海上空850hPa上为西风,200hPa上为东风,活跃期高低空都比非活跃期要暖一些。(3)在多数情况下夏季风和夏季风降水的30-60天的低频振荡比较一致。

The main characteristic of the meridional cell averaged over 110~ 140°E is as follows: The monsoon cell in East Asia replaces Ferrel cell in January and Hadley cell in July in the Northern Hemisphere. In addition, its decadal change is very obvious.

2110~140°E的平均经圈环流主要特点是:1月东亚季风环流圈代替了北半球的Ferrel环流圈,7月东亚季风环流圈代替了北半球的Hadley环流圈,而且其10年际变化也比较明显。

In this paper,mathematical expressions of some swirl characteristic s of typical level hollow swirling flow in inner dissipation discharge tunnel with inlet shaft have been put forward under velocity distribution supposition.

试验观测结果表明,相对于起始断面的各种旋流特性具有明显的分段性质和沿程衰减的特性;下游水位对空腔环流的旋流特性有显著的影响。

As a result, a weak indirect cell is formed in high latitudes. By the 36th time step, the model atmosphere accomplishes the transition form one-cell circulation to two-cell circulation. There is a momentum source in the upper subtropical region. During the transition, the"polar westerlies jet"gets weakened and vanishes at the end, while the subtropical westerlies jet gets strengthened. At this two-cell stage, the generation and dissipation of westerly angular momentum do not balance each other, and the atmosphere is still at an unstable state with great surplus of angular momentum generation.

随着模式的运行,直接环流加强,地表东风带制造西风角动量加大,上支气流的加强,同样在科氏力的作用下,在副热带地区形成副热带西风急流,同时所谓的&极地西风激流&向赤道靠拢、减弱,最后消失,这时在整个半球形成了靠赤道的直接环流和靠极地一侧的间接环流,两圈环流形成的过程仅仅需要9个小时左右。

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