warm cloud 中文意思是什麼
warm cloud
解釋
暖雲-
When rain - cooled downdrafts hit warm air near the ground, a low hanging revolving cloud forms beneath the cell ， a tornado is imminent
當雨冷凝形成的下降氣流遭遇地表暖氣流時- - - - 「超級風胞」下方一股低空旋轉的雲團便已形成，龍卷風就要讓我們大難臨頭了。 -
There is a vaporizing layer below 0 layer and it is far thick, which may be one of the important reasons of small precipitation on ground ; in the paper the cloud and the rain drop size distribution in warm layer of stratiform cloud are calculated and analyzed. it is found that n ( d ) = n0dnexp ( - a d ) can express the size distributions of little cloud drops, big cloud drops and rain drops. the observational and calculated results are well matched
在零度層以下蒸發層的存在，且比較深厚，應是導致地面雨強較小的重要因素之一；本文對暖層的雲滴譜和雨滴譜進行了計算，對小雲滴、大雲滴和雨滴分佈可以用同一種形式的分佈密度函數多階函數n （ d ） = n _ 0d ~ nexp （ - d ）來表示。 -
It was well known that the main process of precipitation formation was collecting cloud water in the warm area and ice phase particles melting in the cold area. positive vertical velocity existed between 700hpa and 500hpa in the warm area and near surface in the cold area. wind convergence existed at the height of 700hpa, and divergence existed above and below the height of 700hpa
通過對降水雲系的綜合研究，建立了河南省春季層狀雲降水概念模型：暖區降水主要通過雲水碰並形成，冷區降水機制以冰粒子融化等冷雲過程為主;暖區700一50ohpa通常有上升氣流，冷區上升氣流分佈在近地面附近: 700沖a存在風場的輻合，其上下則主要是輻散區;水汽主要集中在7o0hpa高度上，暖區水汽來自南、東南方向，冷區水汽以西南輸送為主;暖區位勢不穩定分佈在o 。 -
She could not understand why, stepping out of the window on to the balcony, he smiled under his moustaches and winked so gleefully when a warm, fine rain began to fall on his young oats that were suffering from the drought, or why, when a menacing cloud blew over in mowing or harvest time, he would come in from the barn red, sunburnt, and perspiring, with the smell of wormwood in his hair, and rubbing his hands joyfully would say : come, another day of this and my lot, and the peasants too, will all be in the barn
當他看見溫順的細雨灑在乾旱的燕麥苗上時，他從窗口走到陽臺上，眨著眼，咧開留著鬍髭的嘴唇，她無法明了他怎麼會笑得那麼開心。在割草或者收莊稼的時候，滿天烏雲被風吹散，他的臉曬得又紅又黑汗水淋淋，身上帶著一股苦艾和野菊的氣味，從打穀場回來，這時，她不能理解為什麼他總是高興地搓著手說「再有一天，我們的糧食和農民的糧食都可以入倉了」 。 -
The sunlight gives just about the right warmth, never too warm ; the wind ' s breath is tame, more so because it is blown through those flowery mountain forests, it brings a distant fragrance, together with a slice of damp vapour air, caresses your face, softly engirds your waist, merely taking a simple breath is already an immense delight ; the air is always so clear, no smoke of dwellings in any nearby valleys, not a shred of cloud in the faraway mountains, the totality of this beautiful sight is like a picture unfolding before your eyes, for you to enjoy and appreciate at leisure
陽光正好暖和，決不過暖；風息是溫馴的，而且往往因為他是從繁花的山林里吹度過來，他帶來一股幽遠的澹香，連著一息滋潤的水氣，摩挲著你的顏面，輕繞著你的戶腰，就這單純的呼吸已是無窮的愉快；空氣總是明凈的，近谷內不生煙，遠山上不起靄，那美秀風景的全部正像畫片似的展露在你的眼前，供你閑暇的鑒賞。 -
" the great ambition can sometimes, directly link up the cloud sail toaid the sea ", i sincerely hoped alliance your firm, i surely can by befull warm and the tenacious disposition diligent work, with colleague 精誠 cooperation, for the expensive unit ' s strength of developmentown meagre strength
「長風破浪會有時，直掛雲帆濟滄海」 ，我真誠地希望加盟貴公司，我定會以飽滿的熱情和堅韌的勤奮工作，與同事精誠合作，為貴單位的發展盡自己的綿薄之力。 -
Rainfall is started mainly in cold portions. microphysics for ground rainfall consists of low - level warm portions in which precipitating particles are produced, growing through collision with cloud water and when descending into the warm portions below, ice - phase particles melt and continue to grow by collecting cloud water there. 4 )
降水主要以冷雨過程發動，地面降水形成的微物理過程分別為低層暖雲過程產生並通過碰並雲水增長、降落到暖區的冰相粒子融化和融化的冰相粒子在雲的暖區收集雲水繼續長大等三部分組成。 -
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 tropical warm pool international cloud experiment involves scientists from australia, europe, the united states and japan and aims to find out how the high - altitude cirrus clouds are formed and break up
據路透社1月19日報道，參與該項實驗的科學家們分別來自於澳大利亞美國日本及歐洲等國。科學家們希望通過此舉能弄清高緯度捲雲是如何形成和消散的。 -
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 effect of cloud on ground temperature is akin to wrapping with a blanket to keep our body warm
雲層對地面溫度的影響跟我們蓋被子相似，減低熱能向外散發。 -
In this instance, the warm, saturated air arises from evaporation from the car, forming a cloud when it meets the cold air outside
在這個例子中，暖及飽和空氣b從汽車上蒸發冒出，接解外面較冷空氣s ，形成霧。 -
In this instance, the warm, saturated air ( b ) arises from evaporation from the car, forming a cloud when it meets the cold air ( s ) outside
在這個例子中，暖及飽和空氣（ b ）從汽車上蒸發冒出，接解外面較冷空氣（ s ） ，形成霧。
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