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1)  warm and cold eddies
暖涡及冷涡
2)  cold and warm gyres
冷暖涡
1.
Numerical simulations of the mechanisms of the formations of the South China Sea cold and warm gyres under the joint effects of the wind stress and the coast lines are made in this paper by use of the Princeton University Ocean Model (POM).
利用美国普林斯顿大学海洋模式(POM)对风应力和海岸线共同作用下的南海冷暖涡生成机制进行了数值模拟。
3)  warm eddy
暖涡
4)  cold eddy
冷涡
1.
Sri Lanka cold eddy and its generation mechanism analysis;
斯里兰卡冷涡及其成因分析
2.
Three-dimension temperature structure of cold eddy-upwelling system off northeastern Taiwan Island in summer and winter;
台湾东北海域冷涡-上升流系统冬、夏季温度三维结构
3.
Based on the historical marine observational data, the basic conditions of the cold eddy in the sea area northeast of Taiwan are analysed, which include the seasonal variations, pattern , structure and other characteristics.
根据海洋调查历史资料,对我国台湾东北海域的冷涡基本状况——季节变化、类型、结构与特点进行探讨,主要结果如下:(1)首次提出该海域的冷涡有三处;在春季和夏季,有时出现双涡并存现象。
5)  cold vortex
冷涡
1.
Comparative analysis of two typical hail weather in Ningxia under influence of cold vortex over Mongolia;
蒙古冷涡影响下宁夏两次典型冰雹天气对比分析
2.
Analysis of squall lines occurrign in cold vortexes over Northeast China;
东北冷涡过程中的飑线分析
3.
The rainstorm usually occurs in the developing stage of northeast cold vortex,not in the declining phase.
东北冷涡暴雨一般发生在冷涡发展阶段,冷涡衰退阶段发生暴雨的几率不高,在日常业务预报中往往容易忽视冷涡衰退阶段暴雨的预报,容易出现漏报的现象。
6)  warm-cored vorticity column
暖心涡柱
1.
Its vertical structure is awarm-cored vorticity column with convectional baraclinic distu.
结果指出,与中β尺度雨团相对应的地面气压场上是中尺度低压槽或闭合的中低压系统;在雨团发生初期,其垂直结构为暖心涡柱对流斜压扰动;而在雨团发展期,发展为暖心涡柱强对流混合型低涡;在雨团衰弱期,为暖心涡柱非对流前倾填塞涡。
补充资料:是非涡
1.矛盾纠纷的中心。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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