助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   tropical ocean 在 海洋学 分类中 的翻译结果: 查询用时:0.895秒
图标索引 在分类学科中查询
所有学科
海洋学
气象学
水利水电工程
地质学
生物学
工业通用技术及设备
建筑科学与工程
更多类别查询

图标索引 历史查询
 

tropical ocean    
相关语句
  热带海洋
    Interaction Between Two Polar Heat Sinks and Tropical Ocean Heat Source in Climate System
    气候系统内极区热汇与热带海洋热源之间的相互作用(英)
短句来源
    Reef coral has proved to be an excellent material with which to research into the tropical ocean environment, and its skeletonδ18O is an important tracer for analyzing the recorded environmental information.
    造礁珊瑚是研究热带海洋环境变化的极好材料,珊瑚骨骼δ~(18)O分析是提示其所记录的环境信息的重要手段。
短句来源
    The response of tropical ocean to atmospheric thermal forcing at intraseasonal time scales is numerically studied in this paper. Rossby waves and Kelvin waves are generated in the model ocean.
    利用一个两层半的热带海洋模式,采用数值实验的方法研究了热带海洋对于初始海洋混合层深度异常和大气季节内时间尺度热力强迫激发产生的Rossby波和Kelvin波。
短句来源
    ON THE CORRECTIONS OF VERTICAL VELOCITY AND DIVERGENCE FOR CALCULATING HEAT BUDGET OVER THE TROPICAL OCEAN
    关于在热带海洋与大气间热收支计算中垂直速度和散度的校正
短句来源
    THE INFLUENCE OF TROPICAL OCEAN ON ATMOSPHERIC CIRCULATIONS IN NON-EL NINO PERIODS
    非埃尔-尼诺时期热带海洋对大气环流的影响
短句来源
更多       
  热带海洋
    Interaction Between Two Polar Heat Sinks and Tropical Ocean Heat Source in Climate System
    气候系统内极区热汇与热带海洋热源之间的相互作用(英)
短句来源
    Reef coral has proved to be an excellent material with which to research into the tropical ocean environment, and its skeletonδ18O is an important tracer for analyzing the recorded environmental information.
    造礁珊瑚是研究热带海洋环境变化的极好材料,珊瑚骨骼δ~(18)O分析是提示其所记录的环境信息的重要手段。
短句来源
    The response of tropical ocean to atmospheric thermal forcing at intraseasonal time scales is numerically studied in this paper. Rossby waves and Kelvin waves are generated in the model ocean.
    利用一个两层半的热带海洋模式,采用数值实验的方法研究了热带海洋对于初始海洋混合层深度异常和大气季节内时间尺度热力强迫激发产生的Rossby波和Kelvin波。
短句来源
    ON THE CORRECTIONS OF VERTICAL VELOCITY AND DIVERGENCE FOR CALCULATING HEAT BUDGET OVER THE TROPICAL OCEAN
    关于在热带海洋与大气间热收支计算中垂直速度和散度的校正
短句来源
    THE INFLUENCE OF TROPICAL OCEAN ON ATMOSPHERIC CIRCULATIONS IN NON-EL NINO PERIODS
    非埃尔-尼诺时期热带海洋对大气环流的影响
短句来源
更多       
  热带海洋
    Interaction Between Two Polar Heat Sinks and Tropical Ocean Heat Source in Climate System
    气候系统内极区热汇与热带海洋热源之间的相互作用(英)
短句来源
    Reef coral has proved to be an excellent material with which to research into the tropical ocean environment, and its skeletonδ18O is an important tracer for analyzing the recorded environmental information.
    造礁珊瑚是研究热带海洋环境变化的极好材料,珊瑚骨骼δ~(18)O分析是提示其所记录的环境信息的重要手段。
短句来源
    The response of tropical ocean to atmospheric thermal forcing at intraseasonal time scales is numerically studied in this paper. Rossby waves and Kelvin waves are generated in the model ocean.
    利用一个两层半的热带海洋模式,采用数值实验的方法研究了热带海洋对于初始海洋混合层深度异常和大气季节内时间尺度热力强迫激发产生的Rossby波和Kelvin波。
短句来源
    ON THE CORRECTIONS OF VERTICAL VELOCITY AND DIVERGENCE FOR CALCULATING HEAT BUDGET OVER THE TROPICAL OCEAN
    关于在热带海洋与大气间热收支计算中垂直速度和散度的校正
短句来源
    THE INFLUENCE OF TROPICAL OCEAN ON ATMOSPHERIC CIRCULATIONS IN NON-EL NINO PERIODS
    非埃尔-尼诺时期热带海洋对大气环流的影响
短句来源
更多       
  热带大洋
    Synchronous response of tropical ocean to meridional and zonal wind stress
    热带大洋对纬向和经向风应力的联合响应
短句来源
    The synchronous response of tropical ocean to meridional and zonal wind stress has been studied.
    考虑了经向风应力和纬向风应力联合作用下热带大洋的响应问题.
短句来源

 

查询“tropical ocean”译词为其他词的双语例句

 

查询“tropical ocean”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  tropical ocean
Tropical ocean thermocline variability is studied using gridded data assimilated by an ocean model in the period 1950-2000.
      
Thisthermal energy replenished each day by thesun in the tropical ocean represents atremendous pollution-free energy resourcefor human civilization.
      
Response of the tropical ocean to a uniform zonal wind is studied numerically and analytically.
      
Effect of vertical viscosity and diffusivity on tropical ocean circulation
      
The accuracy of these formulae are validated with respect to air-sea fluxes estimated using the standard algorithm adopted by the Tropical Ocean-Global AtmosphereCoupled-Ocean Atmosphere Response Experiment (TOGA COARE).
      
更多          


In this paper, by using data on monthly mean meridional and zonal windfields of global tropical ocean from 1973 to 1989 (ECMF, KWBC), OLR (CAC), and various subtropical characteristic indexes of the western Pacific Ocean, the influence of the wind field variations in the global tropical ocean on anti-Walker circulation between the Indian Ocean and the western Pacific Ocean, equatorial westerly and air current across the equator is studied, and the physical mechanism of their influence...

In this paper, by using data on monthly mean meridional and zonal windfields of global tropical ocean from 1973 to 1989 (ECMF, KWBC), OLR (CAC), and various subtropical characteristic indexes of the western Pacific Ocean, the influence of the wind field variations in the global tropical ocean on anti-Walker circulation between the Indian Ocean and the western Pacific Ocean, equatorial westerly and air current across the equator is studied, and the physical mechanism of their influence on subtropical ridge reinforcement and westward extension is discussed as well.

本文主要利用1973年以来,全球热带历年逐月各标准等压面月平均风场(ECMWF,KWBC),OLR(CAC)资料及西太平洋副高各种指数(国家气象局),分析了热带风场变异对印度洋-西太平洋反沃克环流、赤道西风、越赤道气流的影响,及其对西太平洋副高脊加强、西伸的影响过程。

By using monthly meridional and zonal wind at grid point of 200hpa and 850hPa level in the global tropical ocean from 1973 to 1989, and at grid point of 10013, 850, 700, 500, 200, 100, 50hPa level from 1980 to 1989, in this paper, the higher and lower layer of troposphere (200, 850hPa) are considered climatically as air current passage across the equator, and the temporal and spatial variation characteristics of the strength for various air current passages across the equator are analyzed. The resultsshow...

By using monthly meridional and zonal wind at grid point of 200hpa and 850hPa level in the global tropical ocean from 1973 to 1989, and at grid point of 10013, 850, 700, 500, 200, 100, 50hPa level from 1980 to 1989, in this paper, the higher and lower layer of troposphere (200, 850hPa) are considered climatically as air current passage across the equator, and the temporal and spatial variation characteristics of the strength for various air current passages across the equator are analyzed. The resultsshow that the air current across the equator in the Eastern Hemisphere is stronger and more stable than that in the Western Hemisphere, and also has obvious seasonal variation. It is further pointed out that air current is transported from the winter hemisphere to the summer hemisphere in the lower layer, conversely from the summer hemisphere to the winter hemisphere in the higher layer, and also indicated the trends of passage intensity variations in the higher layer and lower layer are basically the same. Compared with the higher layer, the passage intensity in the lower layer is more stable and has more evident seasonal variation. The close relationship between air current across the equator and air circulation system are discussed, the results indicate that the annual variations of the various passage intensities reflect the variations of large scale air-sea interactions in the Northern and Southern Hemisphere and is an important information about the global air circulation variability.

本文主要利用1973~1989年逐月全球热带200hPa及850hPa层经、纬向格点风及1980年以来1000,850,700,500,200,100,50hPa各层经纬向格点风,确定了热带对流层高、低(200,850hPa)层具有气候意义的越赤道气流通道,并分析了各越赤道气流通道强度的时、空变化特征。指出东半球比西半球越赤道气流强且稳定,季节变化也较明显。文章还指出,低层东半球向夏半球输送,高层夏半球向冬半球输送,且高、低层各相应通道强度变化趋势基本一致。高层与低层相比较,低层通道强且稳定,季节变化规律也较明显。文章还讨论了越赤道气流与大气环流系统的密切关系,指出各通道强度的年际变化是南、北两半球大尺度海-气相互作用的重要组成部分,是全球大气环流异常变化的重要信息。

In this paper the variations of the wind, temperature,humidity and turbulence in the atmospheric boundary layer over the tropical ocean are analysed by use of observational data with tethersonde over the Equatorial Pacific of 165°E from November 17, 1989 to June 29, 1990. According to the analyses, it is pointed out that generally the thermodynamic structure of the Marine boundary layer in the tropical ocean area remains in a state of convective boundary layer owing to higher temperature of the sea...

In this paper the variations of the wind, temperature,humidity and turbulence in the atmospheric boundary layer over the tropical ocean are analysed by use of observational data with tethersonde over the Equatorial Pacific of 165°E from November 17, 1989 to June 29, 1990. According to the analyses, it is pointed out that generally the thermodynamic structure of the Marine boundary layer in the tropical ocean area remains in a state of convective boundary layer owing to higher temperature of the sea water. Generally, the cumulus generated by local convection easts in the mixed layer, and the cloud top is the top of the mixed layer. The turbulent kinetic energy in the surface layer (less 0. 4 Zi)and in the capping inversion layer is in exceedingly unbalanced state.

StudyonthecharacteristicsofthemarineboundarylayerintheEquatorialPacific¥ZhangZiyuandZhouMingyu(ReceivedAugust21,1993;accepted...

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关tropical ocean的内容
在知识搜索中查有关tropical ocean的内容
在数字搜索中查有关tropical ocean的内容
在概念知识元中查有关tropical ocean的内容
在学术趋势中查有关tropical ocean的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社