wind-field interaction 中文意思是什麼
wind-field interaction
解釋
風場互作用- wind : n 1 風；大風，暴風；氣流；【機械工程】壓縮空氣。2 【航海】上風；風向；〈古語〉〈pl 〉方向。3 氣息...
- field : n 菲爾德〈姓氏〉。n 1 原野，曠野；（海、空、冰雪等的）茫茫一片。2 田地，牧場；割草場；〈pl 〉〈集...
- interaction : n. 1. 相互作用，相互影響，互動。2. 【航空】干擾。
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But in the magnetosphere, weather results from the interaction between the earth ' s magnetic field and the solar wind
但在磁層里，太空天氣卻是由地球磁場和太陽風的交互作用所造成。 -
It also explain that the correlation between ssta of kuroshio and the change of wind field in equaroral mid - pacific is results of air - sea interaction ; however, when time comes into summer, the instance status of ocean is different from the last winter to next early springtime, the sea surface temperature turn into the definitive factor, so the increase of heat flux in may to jun month which is realized by absorbing more heat from the sun radiation results in the decrease of sst in kuroshio in the season of jun - jul. finally, during the aug to dec season of next year, the sst of kuroshio is increasing again
最後分析了黑潮海溫與夏季東亞大氣環流及我國降水的時滯關系，發現：當前冬黑潮區域海溫異常偏高時，後期夏季亞洲低壓的強度減弱，西北太平洋副熱帶高壓強度加強，而且位置西伸、偏北，梅雨鋒位置偏南，長江中下游地區降水偏多，北太平洋冬季海域的海溫分佈呈+ 、 - 、 +趨勢（順序為赤道中東太平洋、西北太平洋、我國近海） ；反之亦然。 -
By using the theoritical analysis, we study the nonlinear interaction between the storm surges and the astronomical tides and the theoritical mode of the storm surges under the control of the wind stress field and the wind pressure field in this paper
本文運用理論分析的方法研究了風暴潮與天文潮的非線性相互作用以及風場、氣壓場作用下的風暴潮波的物理機制問題。本文共分為四章。 -
When the low - tropospheric mpv1 < 0, mpv2 > 0 or negative mpv2 intensify, sudden rainstorm will be inclined to happen. the rainstorm usually happens in the dense section of the negative isoline of mpv1. wind and pressure field on moist isentropic surface reveals that the interaction between cold air and warm air, it successfully explains the reason why " 8
濕等嫡面上風場和氣壓場直觀地揭示了暴雨區冷空氣擴散、暖空氣堆積及兩者在等嫡面上相遇，輻合上升產生暴雨的機制，它較好地解釋了8 . 11 」暴雨強度強，范圍相對較小的原因。 -
This paper studies the interaction relationship between the wind stress ( wind ) field over the tropical pacific and sst by use of the diagnostic analysis and numerical simulation on the basis of sst, 850hpa wind data from ncep / ncar and fsu wind stress data
本文根據ncep / ncar再分析海溫、 850hpa風場資料以及fsu風應力資料，利用診斷分析和數值模擬方法研究了熱帶太平洋風應力（風）場和海溫的相互作用的關系。
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