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- In the lower part of the Ekman boundary layer, for instance, at 20 meter level, the direction of the wind can change about 25 after introducing the thermal wind. 在邊界層下部,例如20米處,引進(jìn)熱成風(fēng)將使風(fēng)向改變達25°左右。
- DYNAMICS OF NON-LINEAR EKMAN BOUNDARY LAYER 非線(xiàn)性Ekman層的動(dòng)力特征
- DYNAMICS OF NON-LINEAR BAROCLINIC EKMAN BOUNDARY LAYER 非線(xiàn)性斜壓Ekman層的動(dòng)力特征
- Time-dependent, coupled, Ekman boundary layer solutions incorporating Stokes drift 加入斯托克斯漂移的依賴(lài)于時(shí)間的耦合?？寺吔鐚咏?/li>
- ON THE CHARACTERISTICS OF THREE-DIMENSIONAL DYNAMICS OF THE NONLINEAR EKMAN BOUNDARY LAYER 非線(xiàn)性大氣Ekman層三維動(dòng)力學(xué)特征
- THE DISSIPATION OF THE ATMOSPHERIC KINETIC ENERGY IN THE LINEAR AND THE SEMI-GEOSTROPHIC BAROCLINIC EKMAN BOUNDARY LAYER 線(xiàn)性與半地轉斜壓Ekman層中大氣運動(dòng)的動(dòng)能耗散
- It is also shown that the Ekman pumping at the top of the boundary layer favors the typhoon acceleration along the local steering current. 邊界層摩擦輻合引起的艾克曼抽吸有利于臺風(fēng)產(chǎn)生沿局地流場(chǎng)引導速度方向的加速度。
- A dynamic study on Ekman characteristics by using 1998 SCSMEX and TIPEX boundary layer data is made. 使用1998年南海季風(fēng)(SCSMEX)試驗和青藏高原科學(xué)試驗(TIPEX)的邊界層資料對Ekman特征進(jìn)行了動(dòng)力學(xué)研究。
- The atmospheric boundary layer is assumed to be separated into two regions ?surface layer and Ekman layer. 利用天氣預報的形勢場(chǎng)計算地轉風(fēng)或梯度風(fēng),以及它與海面摩擦、大氣穩定度的經(jīng)驗訂正關(guān)系。
- Sound Propagation in the Nocturnal Boundary Layer. 夜間邊界層中的聲傳播。
- In this paper, the influence of atmospheric barolinicity on the dynamics of boundary layer with the Ekman momentum approximation is studied. Some new results are obstained. 本文利用Ekman動(dòng)量近似研究了斜壓性對Ekman層動(dòng)力學(xué)的影響,得到了一些新的結果。
- The boundary layer frontalsecondary circulation equation, which is based on the approximation of the Ekman momentum, is usedto make diagnose the synoptical process. 文中還用Ekman動(dòng)量近似導出的邊界層鋒生環(huán)流方程對邊界居中的鋒生環(huán)流做了診斷分析。
- Detection of Boundary Layer Water Clouds by Spaceborne Cloud Radar. 用機載云雷達探測邊界層含水云。
- From the analvtic solutions and the diagram of an example we can see that the present model has some different dynamic characteristics in comparison with the classical Ekman boundary laver model. 由求得的解析解和個(gè)例的圖解均分析得出一些與經(jīng)典Ekman理論很不相同的動(dòng)力學(xué)特征。
- Beyond the boundary layer, the motion is highly irregular. 超出邊界層以外，流體的流動(dòng)非常沒(méi)有規律。
- Formulation of Turbulent Fluxes in the Stable Boundary Layer. 穩定邊界層中湍流通量算法。
- Stull, R.B., 1988: An introduction to boundary layer meteorology. 任平，2003：影響大氣污染物散布的氣象條件。
- Ekman vertical velocity of atmospheric boundary layer was calculated by using GCM data and the new Ekman Pumping formula given by Tan(2000),in which complex boundary was included for stratified atmosphere. 利用GCM模式資料和Tan最新得到的具有復雜邊界的層結大氣邊界層的Ekman泵公式 ,計算了大氣邊界層頂的Ekman垂直速度。
- Combined with Ekman characteristic, we think that the thickness of boundary layer is about 2000m to 2100m in Naqu area in 2004, which is lower than that in most previous researches. 結合Ekman理論;指出2004年那曲地區的大氣邊界層高度為2000-2100m;此高度低于以往多數研究結果.
- As the air proceeds along the test section the boundary layer thickens. 當空氣沿著(zhù)試驗段流動(dòng)時(shí)附面層逐漸變厚。
