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upper circulation
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  上层环流
     The numerical study on the dynamic mechanism of the South China Sea upper circulation in winter
     冬季南海上层环流动力机制的数值研究
短句来源
     The numerical study of the dynamic mechanism of the South China Sea upper circulation in summer
     夏季南海上层环流动力机制的数值研究
短句来源
     RESPONSE OF SOUTH CHINA SEA UPPER CIRCULATION TO MONSOON TRANSITION
     南海上层环流对季风转变的响应
短句来源
     The result by model is also compared with the qualitative analytic result of the density distribution on the isobaric surface and the ADCP data. The results show that they nearly have the same structure, suggesting that the diagnostic result can be used to further study the dynamics of upper circulation variation in the SCS.
     上述计算结果亦与等压面上海水密度分布的定性分析结果及同期观测的ADCP资料进行了比较 ,结果表明模式计算所得到的南海上层环流主要特征与定性分析结果及实测资料大体一致 ,诊断结果可作为南海上层季风环流演变机制研究的依据
短句来源
     An divisional barotropic and baroclinic connection model is employed to study the South China Sea(SCS) upper circulation characteristics and its dynamic mechanism in winter. The results are: (1) In the northern SCS, the flow state is mainly affected by Kuroshio, it is controlled by a cyclonic gyre there except in the continental shelf sea areas to the southwest of Dongsha Islands and adjacent to the west shore of northern Luzon Isalnd where there exists an anticyclonic eddy respectively.
     通过利用一个分区性的正压 -斜压衔接模式来探讨冬季南海的上层环流特征及其动力机制 ,结果表明 :( 1)在南海北部 ,流态主要受黑潮的影响 ,除了东沙群岛西南的大陆架海域以及吕宋岛北部西岸附近各为一反气旋涡外 ,整个南海北部为一气旋式大环流所控制 .
短句来源
  高空环流形势
     The results show that there are many obvious expressions at surface wind frield,upper circulation situation,Q vector divergence,atmospheric stability and energy field,before tronado appearance and at erly period of tronado formation. They may provide forecasting information.
     结果表明:在出现龙卷风之前和形成初期,地面风场,高空环流形势,矢量散度,对流稳定度和能量场诸方面都有表现,可提供预报信息。
短句来源
     We analysis briefly analysed the upper circulation situation and the characteristic of surface pressure field, which resulting in cyclone, so that find out regulation ofcyclone appearance.
     本文简要分析了生成气旋的高空环流形势和地面气压场特征,从而找出气旋发生的规律。
短句来源
     Base on heavy rain data in Kezhou area from the night of 26 to 28 May 2003,the upper circulationground cool airT213-700hPa temperature,T213-850hPa east windand other precipitation condition were analyzed. The reason caused the weather were obtained.
     对2003年5月26日夜间到28日发生在克州地区的大到暴雨天气过程进行了诊断。 分析了高空环流形势、地面冷空气、T213-700hPa湿度场和850hPa偏东风场、降水的物理条件,找出造成此次天气过程的主要原因。
短句来源
  “upper circulation”译为未确定词的双语例句
     DIAGNOSTIC ANALYSIS ON UPPER CIRCULATION VARIATION IN SOUTH CHINA SEA AROUND ONSET OF SUMMER MONSOON IN 1998
     1998年夏季季风爆发前后南海上层环流的诊断分析
短句来源
     According to the analyses of precipitation, temperature, upper circulation field, ocean temperature and other data( 1959-1999) , the main conclusions can be drawn that the more precipitation in summer of 1999 may relate to the following circulation situations, namely, the strong Ural high ridge, the far north position of west Pacific subtropical high ridge line, the far eastward extending west ridge point of it and the strong intensity of polar vortex.
     利用1959-1999年降水、 气温、 高度场等资料分析得出: 1999年夏季青海省多雨与乌拉尔山高压脊偏强、 西太平洋副热带高压位置偏北及西伸脊点位置偏东、  极涡强度偏强等因素有关。
短句来源
     2.The formation of the dense water core and its upper circulation is associated with water masses inter squeezing caused by the development of the Taiwan warm current in spring and summer.
     2.东海高密水核心及其上层环流的形成与由台湾暖流发展引起的水团挤压有关。
短句来源
     Based on analisis of 100mb divergence,geopotential height and vertically -integrated moisture transport fields a discussion is concentrated on features of the upper circulation in the establishment of Asian monsoon in 1979 and in its medium - range oscillation.
     本文主要通过对100毫巴散度场、高度场和垂直积分的水汽输送场的分析,着重讨论了1979年整个亚洲季风区季风建立及其振荡中的高空环流特征。 发现南亚高压周围不同部位的高空辐散场的建立导致了这些地区夏季风的建立,且南亚高压脊线中部和东部散度场具有不同的分布特点。
短句来源
     3.The development of the upper circulation on the East China Sea dense water core area can influence the diffusion of the mixing water off Changjiang mouth.
     3.在春、夏季,东海高密水核心区上层环流的发展可对长江口外混合水(盐度为23~33)的扩散产生很大影响。
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  upper circulation
A three-dimensional baroclinic shelf sea model was employed to simulate the seasonal characteristics of the South China Sea (SCS) upper circulation.
      
Many stand alone modeling studies have been performed to understand subduction and transport pathways in the upper circulation of the Atlantic Ocean.
      
Eventually, the upper circulation returns 2 Sv in layer 3 and 14.2 Sv in layer 2 back to the southern relaxation zone.
      


Based on analisis of 100mb divergence,geopotential height and vertically -integrated moisture transport fields a discussion is concentrated on features of the upper circulation in the establishment of Asian monsoon in 1979 and in its medium - range oscillation.

本文主要通过对100毫巴散度场、高度场和垂直积分的水汽输送场的分析,着重讨论了1979年整个亚洲季风区季风建立及其振荡中的高空环流特征。发现南亚高压周围不同部位的高空辐散场的建立导致了这些地区夏季风的建立,且南亚高压脊线中部和东部散度场具有不同的分布特点。从而使得印度季风有与长江流域梅雨同时开始而与华南雨季降水反位相的特点.在东亚,南亚高压外围东风对于夏季风的向北推进具有很好的指示性。在印度,伊朗高压(南亚高压环流的一部分)外围的东北气流对于印度季风的爆发具有指示性。100毫巴若干地区高度场和亚洲季风区域大范围水汽输送场的40—50天振荡清楚地显示出向东向北移动,而20—30天的散度场的振荡在印度季风爆发后则有系统地向西移动.

In order to reproduce quantitatively the influence of Qinghai-Xizang Plateau on the eastward moving trough (EMT) in winter and to, also, discuss the differences among the terrain impacts under the different circulation, in this paper, the second part of the series papers, a limited area grid point model with 6 levels in the vertical and resolution of 1.875°×1.875°Lon./Lat. in the horizontal is used. According to the demand for the model initial fields and the characters of the Asian upper circulation observed...

In order to reproduce quantitatively the influence of Qinghai-Xizang Plateau on the eastward moving trough (EMT) in winter and to, also, discuss the differences among the terrain impacts under the different circulation, in this paper, the second part of the series papers, a limited area grid point model with 6 levels in the vertical and resolution of 1.875°×1.875°Lon./Lat. in the horizontal is used. According to the demand for the model initial fields and the characters of the Asian upper circulation observed in winter, the idealized initial fields including environmental flow field, characterized by superposed a sine wave shaped trough turbulence on the basic baroclinic westerly flow and westerly Jet, and idealized orographic field are firstly constructed, then a set of 13 experiments, which consist of different member of flow field and orography, are designed. After that, initialization scheme of non-divergence on all levels and fixed lateral boundary condition are utilized to integerate each experiment for 4-5 days. Finally, the behaviour of EMT in each experiment are analysed. The results analysis in the third part of the series papers show that the model is computed stably and the simulated results are reasonable, namely, the idealized initial fields are constructed harmoniously and reasonably, and also argeed quite well with the actual situation. The treatments of lateral boundary condition and initial fields are also appropriate.

为了以数值试验手段定量地再现青藏高原地形对冬季东移大槽的影响,也同时讨论冬季亚洲不同高空环流形势下地形对东移槽影响的差别,本文使用我所6层有限区域格点模式,首先根据该模式对初始场的需要,也源于冬季亚洲地区高空流型的特点,构造了以基本斜压西风气流加高空西风急流,并在其上迭加正弦波槽扰动为主要特征的环境流场等的理想初始场及理想地形场。然后,根据不同流场成员和地形的组合,设计了13个数值模拟试验。接着,利用整层无辐散初始化方案,固定侧边界条件,对各试验积分4—5天,最后分析各试验中东移槽的行为。本研究第三部分的模拟试验结果的分析表明〔19〕,模式计算稳定,模拟结果合理,说明文中理想场的构造是协调的、合理的,也比较接近实际。侧边界条件及初始场的预处理也大体是合适的。

he tronado weather on August 12,1993 in Jinn Province is analysed.The results show that there are many obvious expressions at surface wind frield,upper circulation situation,Q vector divergence,atmospheric stability and energy field,before tronado appearance and at erly period of tronado formation.They may provide forecasting information.

作者对1993年8月12日发生在吉林省境内的一次龙卷风天气进行了分析。结果表明:在出现龙卷风之前和形成初期,地面风场,高空环流形势,矢量散度,对流稳定度和能量场诸方面都有表现,可提供预报信息。

 
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