warm vapor 中文意思是什麼
warm vapor
解釋
低溫水汽-
We can use the mm5 model in definite time, definite area weather forecasting. we conclude that : : the moving route of this necw in its developing progress was direct - south along latitude, the cold air is rough, and just this made the rough vertical velocity ; the necw southern moving and conflicting with the west pacification sub - tropical high makes rough jet steam. the plenty south - west warm and wet air made by the jet stream gave the rainstorm demanded vapor ;. the rough vertical velocity by jet stream is a main reason in this rainstorm ; the mm5 model uses four - direction analysis data as its input, this avoids some errors occurred in observe and transfer, thus made the result more useful
綜合分析認為： （ 1 ） 、這次冷渦在其發生發展過程中，其移動路徑是沿經圈直線南壓，攜帶的冷空氣勢力較強，形成槽后較強的垂直運動； （ 2 ） 、西太平洋副熱帶高壓偏北位置與東北冷渦南壓形成的急流軸，把源源不斷的西南暖濕氣流輸送到遼西地區，也就是急流軸的左前方位置，為這次暴雨的產生提供了充足的水汽來源； （ 3 ） 、低空急流不但為暴雨輸送水汽，其造成的較強的垂直環流也是產生強降水的一個主要原因； （ 4 ） 、 mm5模式以四維同化資料作為初始場，最大限度地避免了觀測誤差可能造成的積分不穩定，提高了模擬結果的參考價值。 -
Warm air can contain more water vapor than cold air.
熱空氣要較冷空氣容納更多的水蒸汽。 -
It seemed a glow to him, a warm and trailing vapor, ever beyond his reaching, though sometimes he was rewarded by catching at shreds of it and weaving them into phrases that echoed in his brain with haunting notes or drifted across his vision in misty wafture of unseen beauty. it was baffling
那東西於他宛若一道微明的亮光，一片溫馨的流雲，永遠可望而不可即，他偶然抓住了一絲半縷編織成幾個詩句，那維繞的音韻便在他腦子里回蕩往復，而那以前從未見過的芙便如膝俄的霧雷在他的視野中涌現。 -
The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows, so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening, one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea. furthermore, with the effect of terrain, the southern shaanxi province became the center of this extremely heavy rain process
中尺度結構分析表明，本次暴雨具有明顯的中尺度特徵，是由三支氣流共同作用的結果，分析發現（ 1 ）地面東南風和地形在這次大暴雨過程起主要作用； （ 2 ）東路冷空氣主要是通過中低層侵入陜南地區的，並與地面冷式錮囚鋒的形成密不可分； （ 3 ）夜博士論文:中尺度地形對陜南暴雨的影響研究間垂直次級環流發展加強可能有兩個原因，一個是由於地形山谷風的作用，另一個是降水的潛熱釋放激發了上升運動: （ 4 ）位勢不穩定層結的形成與低層暖濕平流的發展有很好的對應關系; （ 5 ）本次暴雨的水汽主要靠偏南風急流將孟加拉灣和中國南海的水汽輸送至西北地區東部，為暴雨的發生提供了必要熱力條件。 -
Rain occurs when a mass of warm air laden with water vapor rises
當滿含水汽的暖空氣團上升時，就會下雨。 -
The findings show that there exists overlap between macroscale convergence and warm advection if the degree of clock - wise turn dosen " t keep constant on both sides of zero doppler velocity contour about the near range of the observational site. the overlap produces vertical vapor transport and upward convergence movement favorable for formation and continuation of rain gush
結果表明：零速度帶在測站近距離兩側的彎曲程度不一致是暖平流與大尺度輻合運動的迭加所造成，這一結構為暴雨產生和維持提供了有利的水汽垂直輸送和輻合上升運動。 -
Potential instability existed near 0 in the warm area and between - 10 and 0 in the cold area. the occurrence of potential instability was corresponding with maximum rainfall and maximum vapor content
C附近，冷區位勢不穩定分佈在一10一ooc ，位勢不穩定出現的時間與地面強降水、水汽最大累積區出現的時間一致。 -
Three passages of vapor transfer are related to the regional precipitation, especially the one carrying water from the bay of bengal. mixed cold and warm cloud portions are favorable for " catalysis - water supply ". the duration and rainfall - hit area are about half the lifecycle and rainbelt size, respectively
；降水天氣的主要水汽輸送路徑有三條，以來自孟加拉灣的西南水汽輸送帶對降水最為有利；雲系以冷暖混合雲體為主，具有發生「播撒-供應」機制有利的宏觀雲體條件；雲系降水的時段和面積一般只有雲系生命期和面積的一半。 -
The sauna center which provides chinese and thai massage, vapor bath, cool room, warm & cold pools is an elegant style place for your leisure
極盡豪華的健康中心。包括干濕蒸氣浴、冷凍房、冰凍房、冰熱藥物水池、中泰式按摩、健身及美發。當地最大型的水池區是您舒展身心、享受悠閑的最佳選擇。 -
System provide superiority momentum and middle - level dry and cold atmosphere for the hailstone convection. the ground pressure field and wind field provide low layer warm and humid condition. the second part is simulating water vapor combine conditions
此次冰雹強對流天氣過程主要是受深厚的低渦天氣系統作用的結果，為此次天氣過程提供了優越的動力條件，有利於對流層低層暖濕空氣的抬升和中層乾冷空氣的注入。
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