cold advection中文是什么意思

發(fā)音:

中文翻譯
造句

冷平流

cold adj. 1.冷，寒，凍；冰涼的。 2.冷靜的，冷淡的， ...
advection n. (熱的)對流；(空氣的)平流。 adj. -vec ...
advection n. (熱的)對流；(空氣的)平流。 adj. -vective
advection cooling 平流冷卻
advection fog 海面霧; 平另; 平流霧
advection heat 對流熱
advection inversion 平流逆溫
advection layer 平流層; 平流運(yùn)動層
advection of heat 平流熱效
advection region 平流區(qū)
ageostrophic advection 非地平流
differential advection 差異平流
geostrophic advection 地轉(zhuǎn)平流
horizontal advection 水平平流
temperature advection 溫度平流
thermal advection 熱平流; 溫度平流
thickness advection 厚度平流
vertical advection 垂直平流
vorticity advection 渦度平流
warm advection 暖平流
advection radiation fog 平流輻射霧
cyclonic vorticity advection 氣旋式渦度平流
differential thermal advection 差異熱平流
geostrophic advection scale 地轉(zhuǎn)平流尺度
thermal vorticity advection 熱成渦度平流; 熱力渦度平流

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例句與用法

The results show that a warm high ridge at the middle level and transformed surface cold high over the plain provide a good background condition ; a cooling process produced by net surface radiation fluxes is the trigger and strengthening mechanism for the fog event ; the subsidence flow at the middle and low tropospheric levels is favorable for the setting - up and maintenance of stable stratification at the boundary layer and weak wind condition at the ground layer over the fog region ; the transportation of weak warm advection at lower levels and weak lift motion at the boundary layer play a very important role to the long maintenance of the fog event ; the intrusion of north wind accompanied by cold advection is a main dynamic factor of the fog dissipation
結(jié)果表明：在中高層暖性高壓脊及地面變性冷高壓穩(wěn)定維持的大尺度背景條件下，地表凈輻射引起的近地層冷卻是大霧過程的觸發(fā)和加強(qiáng)機(jī)制；中低空下沉氣流的存在有助于近地層的弱風(fēng)條件和穩(wěn)定層結(jié)的建立；低層暖平流的輸入和邊界層的淺層抬升是大霧長時間持續(xù)的原因；伴隨冷空氣南下的偏北大風(fēng)是驅(qū)使大霧消散的動力因子。
There are two parts in this paper : firstly , a set of single doppler velocity models are presented for typical ambient windfields that include those of being uniform horizontally , macroscale convergence and divergence , which overlap warm and cold advection . which are marked by different signatures in the single doppler velocity field . the models proposed can help users identify useful information from the dopple velocity patterns
本論文包括兩個部分：第一篇通過對典型風(fēng)場的單多普勒天氣雷達(dá)徑向速度圖象進(jìn)行模擬，典型風(fēng)場包括水平均勻一致的風(fēng)場、非均勻水平風(fēng)場的大尺度運(yùn)動的輻合輻散風(fēng)場以及大尺度運(yùn)動的輻合輻散風(fēng)場與冷暖平流的迭加等。

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