rossby waves 中文意思是什麼
rossby waves
解釋
羅斯貝波-
Firstly, this paper designs a polar coordinate barotropic vorticity equation semi - spectral model and a quasi - geostrophic grid model in order to research the propagation of vortex rossby waves and tropical cyclone intensity change entirely
本文首先設計了一個極坐標系正壓渦度方程的半譜模式、一個準地轉格點模式對渦旋rossby波傳播和熱帶氣旋強度變化進行了較為系統的研究。 -
There is teleconnection relations between shandong summer rainfall and the convective activities happening in tropical areas in spring and summer accomplished by rossby waves
通過分析強弱季風年春、夏季熱帶地區olr場的分佈特徵，發現熱帶地區的對流活動與山東夏季降水之間存在著遙相關關系。 -
Taking months to traverse the pacific, rossby waves march to the western boundary of the pacific basin, which is modeled as a smooth wall but in reality consists of quite irregular island chains, such as, the philippines and indonesia
用了幾個月橫穿太平洋， r波到達太平洋海盆的西部邊界，被模擬成一堵平滑的墻壁，但是實際上，是由很不規則的島嶼鏈組成，比如，菲律賓群島和印度尼西亞群島。 -
Secondly, a shallow - water model is designed to study the topographical effects on the propagating vortex rossby waves and tropical cyclone intensity change detailedly
之後設計了一個淺水模式較詳細地研究地形對渦旋rossby波傳播以及熱帶氣旋強度變化的影響。 -
The main conclusions show as following : 1 the effects of propagating vortex rossby waves on tc intensity change are relative closely to the position, the size and intensity of the initial disturbance
主要結果可歸納如下： 1渦旋rossby波傳播對熱帶氣旋強度變化的影響，與初始擾動相對渦旋中心的位置、初始擾動尺度大小及強度等關系密切。 -
Montgomery and kallenbach proposed that the propagation of vortex rossby waves may intensify the tropical cyclone, this new physical mechanism has been widely studied
Montgomery和kallenbach提出，渦旋rossby波傳播可使熱帶氣旋加強，這一新的物理機制得到了廣泛的研究。 -
Being a new mechanism of typhoon intensity variation including intensity mutation and a leading task in typhoon dynamics, vortex rossby waves ( referred as vrw hereafter ) theory was studied in depth by professor montgomery and his students of colorado university
渦旋rossby波（ vrw ）理論是臺風強度變化包括強度突變的一種新機制，是目前臺風動力學的一個前沿課題。美國科州大學montgomery教授和他的學生們對此進行了深入的研究。
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