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tropical easterly jet
相关语句
  热带东风急流
     A Climatological Study on the Tropical Easterly Jet and Asian Summer Monsoon
     热带东风急流及亚洲夏季风的气候学研究
短句来源
     In this paper, studies are made of the structure and interannual variation of the 500hPa teleconnection between the Bay of Bengal(15°N, 85°E) and the Sea of Japan(40°N, 130°E) during the Northern early autumn and its relation to tropical easterly jet, El Nino and China's precipitation.
     研究了北半球初秋(9月)500hPa孟加拉湾(15°N,85°E)与日本海(40°N,130°E)的遥相关结构、年际变化及其与热带东风急流、厄尔尼诺事件、中国降水的关系.指出,当孟加拉湾500hPa高度上升时,日本海高度下降。
短句来源
     Based on NCEP/NCAR reanalysis data, the structure and variation of Tropical Easterly Jet (TEJ) 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. Finally, the difference between NCEP/NCAR and ERA-40 reanalysis data is made for reference.
     本文主要是用NCEP/NCAR再分析资料研究了热带东风急流(TEJ)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。
短句来源
  “tropical easterly jet”译为未确定词的双语例句
     A Study of the Tropical Easterly Jet Stream Over Asia and Africa
     热带东风喷射气流之天气学研究
短句来源
     After analyzing the circulation fields and divergence fields of both 150-100 hPa and 200 hPa,however,we found out that the level of 200 hPa could not reflect the real change of the upper-tropospheric circulation of Asian summer monsoon,especially the characteristics and variations of the tropical easterly jet which is the most important feature of the upper-tropospheric circulation and whose core is located in the layer of 150-100 hPa.
     WYI定义为850与200 hPa的纬向风差,但通过分析150—100 hPa和200 hPa的环流场、散度场与垂直运动场,发现200 hPa层并不能真正反映亚洲季风系统上层环流的变化,尤其是其最主要的环流特征即热带东风急流的变化,其核心位于150—100 hPa。
短句来源
     THE DIAGNOSTIC ANALYSIS OF THE MAINTAINING MECHANizM OF THE UPPER TROPICAL EASTERLY JET
     热带高空东风急流维持机制的诊断分析
短句来源
     In this paper, the struoture of the tropical easterly jet is analysed by using FGGEⅢB data. The investigation of angular momentm budget shows that the divergence of the horizontal momentum flux in the high troposphere affected by the mean meridional monsoon circulation is a dynamic factor in maintaining the easterly jet.
     本文利用FGGEⅢB资料,分析了热带东风急流的结构和角劝量收支,表明平均绝对角动量水平通量辐散是维持东风急流的动力因素,影响这种辐散是平均的季风经圈环流;
短句来源
     In this paper,the struoture of the tropical easterly jet is analysed by using FGGEⅢB data. The investigation of angulan momentm budget shows that the divergence of the horizontal momentum flax in the high troposphere af- fected by the mean meridional monsoon circulation is a dynamic factor in ma- intaining the easterly jet.
     本文利用 FGGEⅢB 资料,分析了热带东风急流的结构和角动量收支,表明平均绝对角动量水平通量辐散是维持东风急流的动力因素,影响这种辐散是平均的季风经圈环流;
短句来源
  相似匹配句对
     The Nonlinear Process of the Depression Formation in the Tropical Easterly Flow
     热带东风气流中低压形成的非线性过程
短句来源
     Then the depression formation in tropical easterly flow is discussed.
     由此讨论了热带东风气流中的低压形成。
短句来源
     THE DIAGNOSTIC ANALYSIS OF THE MAINTAINING MECHANizM OF THE UPPER TROPICAL EASTERLY JET
     热带高空东风急流维持机制的诊断分析
短句来源
     A Climatological Study on the Tropical Easterly Jet and Asian Summer Monsoon
     热带东风急流及亚洲夏季风的气候学研究
短句来源
     A Study of the Tropical Easterly Jet Stream Over Asia and Africa
     热带东风喷射气流之天气学研究
短句来源
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  tropical easterly jet
The results show that the radiative transfer is essential in maintaining the intensity of the low level Somali Jet as well as the upper level Tropical Easterly Jet (TEJ) over the Indian sub-continent and adjoining seas.
      
These high winds have been found as a unique phenomenon distinct from a jet stream and therefore it is considered appropriate to call them Tropical Strong Easterlies (TSE) rather than as a tropical easterly jet stream.
      
On finding these current concepts questionable, this study offers an alternative explanation for the migration of the upper tropospheric anticyclone to the Tibetan Plateau and also for the development of the tropical easterly jet.
      
This paper, however, assesses the role of an upper troposphere synoptic feature of importance in modulating surface rainfall over Sudan in the eastern Sahel: the Tropical easterly Jet (TEJ).
      
The Tropical easterly Jet and Sudan rainfall: A review
      
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The FGGE Ⅲ-b data compiled by ECMWF of the July 1979 is used to diagnose the kinetic energy (KE) budget of the tropical flow. The results reveal that the horizontal distribution of the mean flow KE is very similar to that of mean KE. This similarity indicates that the major features of the tropical summer circulation are standing eddy phenomenas. The transient KE formed two hemispheric interaction channels near 105°E and 150°E at 850 hPa and near 150°E and 30°W at 200 hPa. Also, large value transient KE occurred...

The FGGE Ⅲ-b data compiled by ECMWF of the July 1979 is used to diagnose the kinetic energy (KE) budget of the tropical flow. The results reveal that the horizontal distribution of the mean flow KE is very similar to that of mean KE. This similarity indicates that the major features of the tropical summer circulation are standing eddy phenomenas. The transient KE formed two hemispheric interaction channels near 105°E and 150°E at 850 hPa and near 150°E and 30°W at 200 hPa. Also, large value transient KE occurred over the mid-ocean trough areas, the so called "storm track".At 850 hPa, Somali jet is the main circulation system which generates KE. At 200 hPa, the generation is positive (negative) in the upstream (downstream) region of the tropical easterly jet. It indicates that the kinetic energetics of the easterly jet is similar to that of the westerly jet in the mid-latitude.In the Afirica-Arabian Sea monsoon region, the net generation of KE (KE generation plus KE flux divergence) is negative in the upper troposphere. While in the Bay of Bangel-South China Sea region the net generation is negative in the lower troposphere. Such deficiencies of KE may be compenseted by the vertical transport of KE, i. e., the vertical coupling of the upper and lower tropospheric flow is quite important in the monsoon area.

应用欧洲中期预报中心的FGGEⅢ-b个客观分析资料计算了1979年7月热带大气的动能平衡。热带环流系统的动能主要集中在定常涡旋部分。对流层下层,105°E和150°E为两半球间瞬变涡旋的通道。对流层上层,瞬变涡旋的通道和洋中槽相联系,位于150°E和30°W附近。 索马里急流是对流层下层制造动能的主要环流系统。对流层上层,南亚东风急流入口区制造动能,出口区破坏动能,其动能收支与中纬度西风急流相似。 非洲-阿拉伯海季风区和孟加拉湾—南海季风区的动能平衡很不相同。动能的垂直输送可能在季风环流中很重要。

In this paper, the struoture of the tropical easterly jet is analysed by using FGGEⅢB data. The investigation of angular momentm budget shows that the divergence of the horizontal momentum flux in the high troposphere affected by the mean meridional monsoon circulation is a dynamic factor in maintaining the easterly jet. The jet is closely related to the mean maridional tempereture gradient. The tempereture gradient in the middle high troposphere is affected by the heating field. Therefore,...

In this paper, the struoture of the tropical easterly jet is analysed by using FGGEⅢB data. The investigation of angular momentm budget shows that the divergence of the horizontal momentum flux in the high troposphere affected by the mean meridional monsoon circulation is a dynamic factor in maintaining the easterly jet. The jet is closely related to the mean maridional tempereture gradient. The tempereture gradient in the middle high troposphere is affected by the heating field. Therefore, the heating caused by the monsoon trough and ITCZ is an important thermodynamical factor affecting the intensity of the jet.

本文利用FGGEⅢB资料,分析了热带东风急流的结构和角劝量收支,表明平均绝对角动量水平通量辐散是维持东风急流的动力因素,影响这种辐散是平均的季风经圈环流;就热力而论,急流与正的南北向平均温度梯度相关,而影响对流层中高层温度梯度的重要因素是南北向不同的加热作用。由季风槽和ITCZ引起的加热,是影响急流强度重要的热力因子。

In this paper,the struoture of the tropical easterly jet is analysed by using FGGEⅢB data.The investigation of angulan momentm budget shows that the divergence of the horizontal momentum flax in the high troposphere af- fected by the mean meridional monsoon circulation is a dynamic factor in ma- intaining the easterly jet.The jet is closely related to the mean maridional temperature gradient.The tempereture gradient in the middle high troposphere is affected by the heating field.Therefore,the...

In this paper,the struoture of the tropical easterly jet is analysed by using FGGEⅢB data.The investigation of angulan momentm budget shows that the divergence of the horizontal momentum flax in the high troposphere af- fected by the mean meridional monsoon circulation is a dynamic factor in ma- intaining the easterly jet.The jet is closely related to the mean maridional temperature gradient.The tempereture gradient in the middle high troposphere is affected by the heating field.Therefore,the hoating caused by the monsoon trough and ITCZ is an important thermodynamical factor affecting the intensity of the jet.

本文利用 FGGEⅢB 资料,分析了热带东风急流的结构和角动量收支,表明平均绝对角动量水平通量辐散是维持东风急流的动力因素,影响这种辐散是平均的季风经圈环流;就热力而论,急流与正的南北向平均温度梯度相关,而影响对流层中高层温度梯度的重要因素是南北向不同的加热作用。由季风槽和 ITCZ引起的加热,是影响急流强度重要的热力因子。

 
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