warm rain 中文意思是什麼
warm rain
解釋
暖雨-
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。 -
Tea mountain of yiwu is a high mountain with heavy fog, fertile land, warm temperature with more rain, is the wonderful place where produces the first - class tea, top class of grandifoliate planted tea of yiwu attaches the chun yi ming with the time - honored and innovated traditional tea producing technology, provides the non - forgettable excellent tea products for people
易武茶山山高霧重，土地肥沃，溫熱多雨，是產上等茶葉的極品之地，易武上品野生古樹茶輔以淳一茗歷經革新的傳統制茶工藝，生產出讓人難以忘懷的絕妙茶品。 -
In winter, rain is usually brought about when warm and cold air masses meet
2003年1月6日在冬季，雨一般是由冷暖氣團相遇所引起。 -
The paper concludes that the changing rate of ndvi of rain forest in tropic is the smallest, the changing curve is smooth, while the changing rate of ndvi of the deciduous broad leaf forest in warm - temperate zone is the largest the change of ndvi is the most conspicuous in winter and spring ( especially in april ) while is not conspicuous in summer and autumn by analyzing the change of ndvi along latitude using the ndvi value of different vegetation types along the same longitude. the vegetation index from warm temperate zone to semitropical zone has obvious transition, while other areas have no distinct change by analyzing the change of ndvi from temperate zone to semitropical zone to tropical zone using ndvi averagejn the same time it is concluded that the sink value in the beginning of the year 1995 is from the influence of the monsoon in east of china by analyzing the ndvi curve of several typical needle leaf forests. the relation between ndvi value and temperature is conspicuous while the relation of precipitation is less or not by analyzing the relation between ndvi and temperature and precipitation finally it can get the conclusion that the change of river area is the smallest, the change of sienna area is the greatest by analyzing two phases of tm data in 1987 and 1997 with rs technic
利用從同一經度的不同森林類型ndvi值分析，沿緯度方向ndvi變化可得出， ndvi在冬春季變化最明顯（尤其是在4月份最大） ，而在夏季和秋季變化不明顯。利用ndvi均值進行分析，從暖溫帶到亞熱帶到熱帶的變化情況發現，從暖溫帶到亞熱帶ndvi指數形成明顯的階躍，而其它區域沒有太大的變化，同時對幾種典型的針葉林曲線分析可知其年初的凹值源自於我國東部季風的影響。利用ndvi數據分析其與月均溫度與降水的相關性得出與溫度相關性較為顯著，而與降水相關性不顯著或無相關性。 -
Spurts of warm rain blew fitfully against their faces.
陣陣溫熱的雨點拍打在他們臉上。 -
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。 -
Given the present unusual global warming rate on an already warm planet, we can anticipate that areas with summer melt and rain will expand over larger areas of greenland and fringes of antarctica
在已經很暖的地球加上現在不尋常的全球暖化速率，我們可以預期，在格陵蘭與南極的邊緣，夏季融冰與降雨的地區會大幅擴張。 -
The weather is warm and sunny here. do you get much rain
這里的氣候溫和，陽光充足。你們這兒雨水多嗎？ -
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 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。 -
The world is beautiful, because of warm sunshine and also because of its rain and storm
這個世界是美麗的，因為它既有煦暖的陽光，也有風雨和冰雪。 -
The warm and comfortable rain soaked into the ground and from the branches continually hung the countless drops, glistening in the succeeding sun.
溫暖而舒適的雨水滲入土地，樹枝上仍掛著數不清的雨點，在雨後的陽光下閃閃發光。 -
Because of nanyue mountain ( chang shou - shan ), shek kwu college ( song taizong treason 2003, the national academy of four ), with wang chuan, cai lun, fu li, peng yu - scales, and other celebrities and the birth of the precipitation value xiang cultural uniqueness yanfeng rain, shek kwu jiangshan, anther spring river, xue - ling yue ping, zhu ling shidong, grass white wine bridge home, the west lake night - white lotus, look at the east, and warm peach wave steaming mountain city shigu, hunan, lei sanshui in this intersection and the huang director
因受南嶽衡山（五嶽壽山） 、石鼓書院（宋太宗至道三年，全國四大書院之一）影響，隨著王船山、蔡倫、李芾、彭玉鱗等眾多名人的誕生而沉澱了衡湘文化的精髓，雁峰煙雨、石鼓江山、花藥春溪、岳屏雪嶺、朱陵詩洞、青草橋頭酒白家、西湖夜放白蓮花、細看東州桃浪暖及市內石鼓山下蒸、湘、耒三水在此交匯而名遐三湘。 -
Based on t213 and other observational datasets, a severe heavy rain occurred in changjiang - huaihe basins during 4 - 5 july 2003 is studied. the primary diagnostic analyses show that double or single block is the characteristics of the macroscale circulation in this rainfall process. the strong conflict of warm and cold mass, mesoscale convergence on meiyu front, shear line, and stably maintaining of high and low jets make for the rainfall
本文採用地面高空常規資料，每6h一次的降水資料，以及t213數值預報資料，對2003年7月4 - 5日發生在江淮地區的一次梅雨鋒暴雨過程的影響系統及其可能機制進行了初步的診斷分析，發現，高緯雙阻、單阻形勢是這次暴雨過程發生的大尺度環流特徵；冷暖空氣的激烈交鋒、梅雨鋒上的中尺度輻合線、 700hpa 、 850hpa上的低渦、切變線以及穩定維持的高低空急流是導致這場暴雨的直接影響系統；該地區維持一個高能、飽和、潛在不穩定的環境，有利於特大暴雨的產生和維持。 -
Heavy rainfall occurred in the warm area, and maximum rainfall lay in the windward slope where the width of raindrop size distribution was b roadened and sometimes it was bimodal spectrum. the shape of rain band in cold area was zonal, and the area of rain band was small
暖區有明顯的強降水中心，雨強極大值出現在山區迎風坡，降水雨滴譜譜寬較大，有時滴譜呈雙峰型分佈；冷區降水區常呈帶狀分佈，雨區范圍大，雨滴譜較窄，雨滴譜為單峰型。 -
I wonder if love is the sun shine flowers, warm rain xiaocaohu also all over her
關愛的陽光不知是普照鮮花，溫馨的雨露也要灑遍小草。 -
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。 -
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。 -
As the weather grew warmer it was not sensibly worn away by the water ， nor broken up and floated off as in rivers ， but ， though it was completely melted for half a rod in width about the shore ， the middle was merely honeycombed and saturated with water ， so that you could put your foot through it when six inches thick ； but by the next day evening ， perhaps ， after a warm rain followed by fog ， it would have wholly disappeared ， all gone off with the fog ， spirited away
因為天氣更溫暖了，它不再給水沖掉，也不像河裡的冰那樣地浮動，雖然沿岸半桿闊的地方都已經溶化，可是湖心的依然像蜂房一樣，飽和著水，六英寸深的時候，還可以用你的腳穿過去；可是第二天晚上，也許在一陣溫暖的雨和緊跟著的大霧之後，它就全部消失，跟著霧一起走掉，迅速而神秘地給帶走了。 -
From there you might stand in a light warm rain as you look out over the beautiful valleys below
在那裡當你俯視下面美麗峽谷的時候，你可能與一場柔和溫暖的小雨之中不期而遇
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