stratus cloud 中文意思是什麼
stratus cloud
解釋
層雲-
By comparing model simulation with an observed precipitation formed by stratus cloud system, the new scheme shows the improvement of prediction precipitation
利用新方案模擬了一次層狀雲降水過程，新舊方案降水模擬結果的對比表明新方案的降水預報效果有所改進。 -
These results suggest that the new scheme will provide some valuable information on macro and micro structure characteristic of stratus cloud, physical process of precipitation and weather modification research
說明新方案可以為層狀雲的宏微觀結構特徵、降水物理過程和人工影響研究提供一定依據。 -
The width of raindrop size distribution in the warm area was narrow and its shape was single model. simulating results of one - dimension stratus model showed that the content of cloud water that grew up by deposition process was the largest in the warm area, and cloud water existed between 2km and 6km. in the warm area, the formation of rain water which existed between 1km and 4km was behind of the formation of cloud water, and the development of rainwater was depend on collecting cloud water
一維層狀雲模式模擬結果表明，暖區以凝華增長的雲水為主，雲水分佈在2 6km高度；雨水在雲水形成后產生，分佈在1 4km之間，主要通過碰並雲水增長；霰在雨水形成后產生，主要通過碰並雲水增長，分佈在雲水區的中下層，霰形成后，雨水主要由霰融化產生。 -
The macro characteristics of status cloud systems have been studied by using every 3 - hour sounding data, satellite cloud pictures, radar echoes, synoptic charts, surface rainfall, raindrop size distribution and microwave radiometer. the spatial distribution of precipitation particles and the mechanisms of their formation were studied by one - dimension stratus model. thus, spring stratus precipitation conceptual model was primarily established in henan province
利用3小時一次的加密探空資料、衛星雲圖、雷達回波圖、天氣圖、地面雨量、雨滴譜、微波輻射計等資料，分析了降水雲系的宏觀特徵，並利用一維層狀雲模式研究了降水粒子的時空分佈和水質粒形成的微物理特徵，由此初步建立了河南省春季層狀雲降水的概念模型。 -
Analyzed results of macro observed data showed that the configurations of stratus cloud systems were inhomogeneous, and stratus cloud systems consisted of several single clouds. different clouds were departed by obvious borderline, and the height of cloud top changed between 4 and 8km. the height of 0 level occurred at about 3. 5km height which was meant that super - cold cloud existed
由觀測資料分析可知，河南省春季層狀雲系結構不均勻，雲系由若干個雲塊組成，雲塊之間有明顯的界線，雲頂高度在4 8km之間起伏變化，零度層亮帶高度約為3 . 5km ，雲系存在一定厚度的過冷雲層。 -
The output of the new scheme could give reasonable microstructure of cloud and indicate some characteristics of stratus cloud, which enhances the capability of mm5 to study the cloud microphysical process. the numerical simulation reveals the possible mechanism of the rainfall by one station microphysical process analysis
模擬給出了雲的合理微觀結構，揭示了層狀雲的一些特徵，增強了mm5研究微觀雲物理的能力；通過單站微物理過程分析，揭示了降水過程的可能形成機制。
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