暖區 的英文怎麼說

中文拼音 [nuǎnqū]
暖區 英文
warm saw
  • 暖 : Ⅰ形容詞（暖和） warm; genial Ⅱ動詞（使東西變熱或使身體變溫暖） warm up
  • 區 : 區名詞（姓氏） a surname
  1. Taking loess cave dwelling of yan an area as represen t area ， the annual temperature wave inside the cave dwelling are solved under t he annual temperature wave of outside disturbance in yanan furthermore ， by comparing with that of bungalows ， the characteristics that warm in winter and cool in summer in cave dwelling are illustrated in quantity

    以延安地區黃土窯洞為模型，以當地的室外年溫度波為外擾，用反應系數法求解和分析了窯洞室內的年溫度變化;並與相同空間結構，相同外擾作用下的平房作了分析比較，定量的說明了窯洞與平房相比具有冬暖夏涼的優點。
  2. Climbing ferns ferns of the family schizaeaceae, found in most parts of the world in warm and tropical regions, including north america

    攀援蕨類：分佈於溫暖的熱帶區域的蕨類，北美洲也有分佈。
  3. Change of cold wave in dalian under global warming condition

    全球變暖背景下大連地區寒潮活動的氣候變化
  4. With the support of the chiayi municipal government, fellow initiates from the chiayi center invited community organizations in the area, including the international tong - jee society, the chiayi lions club, and the seeu - lan culture and education foundation, to cosponsor an activity entitled " heartwarming winter - love on earth. " together, they paid visits to senior citizens in the home of love, the home of compassion, and the home of jee - may care. lucky money was presented to the seniors as gifts for the lunar new year

    嘉義小中心今年首度邀請國際同濟會國際嘉義獅子會及秀巒文教基金會等嘉義地區民間社團，在嘉義市政府的督導之下，聯合舉辦寒冬送暖天地有情，人間有愛慰問老人活動，前往嘉義市仁愛之家博愛仁愛之家以及濟美仁愛之家，致贈年節慰問金，並以歌舞才藝表演，讓老人們度過一個溫馨的季節。
  5. At first, analysis of extreme temperature ' s spatial distribution of variety trend shows that the minimum temperature in the north are going up while the maximal temperature in east china declining widely, which is a numerical characteristics of prevailing warmer - winter in recent years. so the change of minimum and maximal temperature are dissymmetrical

    首先從總體上，分析極端最高和極端最低溫度變化趨勢的空間分佈：北方地區極端最低溫度普遍上升，且幅度較大，是近年來暖冬盛行的一個數值化特徵；極端最高溫度在東部普遍下降，最低最高溫度變化具有不對稱性。
  6. He had sometimes propelled her on warm summer evenings, an infirm widow of independent, if limited means, in her convalescent bathchair with slow revolutions of its wheels as far as the corner of the north circular road opposite mr gavin low s place of business where she had remained for a certain time scanning through his onelensed binocular fieldglasses unrecognisable citizens on tramcars, roadster bicycles, equipped with inflated pneumatic tyres, hackney carriages, tandems, private and hired landaus, dogcarts, ponytraps and brakes passing from the city to the phoenix park and vice versa

    有時在溫暖的夏日傍晚，布盧姆把這位多少擁有一些資產足以自立的病孀扶到康復期患者坐的輪椅上，慢慢地將她推到北環路拐角處加文洛68先生的牲畜交易場所對面。她在那兒逗留上半晌，隔著他那架單鏡頭雙筒望遠鏡眺望那些難以辨認的市民們：他們搭乘電車氣胎打得鼓鼓的自行車出租馬車雙駕馬車自家用或租來的四輪馬車單馬拉的雙輪馬車輕便小馬車和大型四輪游覽馬車，在市區與鳳凰公園之間穿梭著。
  7. I went in for pathetic trysts in poorly heated east end flats

    我到供暖很差的倫敦東部的貧民區去約會
  8. Firstly, evidence from depositional pattern suggests that the hsl has experienced an expansion - contraction circle since the late glacial epoch. the expansion and movement of the hsl or desert in early stage were clearly marked by the presence of paleo - aeoline sands. the occurrence of paleosoal characterized the stabilization and contraction of the hsl and also indicated the activity of pedogenesis on the paleo - aeilian sands

    通過系列氣候代用指標的分析，首次發現該地區粒度、磁化率指標值在兩個大的峰值之間有多個小的峰谷出現，表明了在大的氣候變化階段次一級的暖濕?乾冷氣候波動，值的進一步做年齡的小尺度高解析度研究。
  9. The ncep / ncar globally tropospheric 1 1 reanalysis data have been employed to select six landfall typhoon cases in order to diagnose variations of typhoon warm sectors in atmospheric boundary layer during their whole life periods

    摘要採用ncep / ncar全球對流層1 1再分析格點資料，選取6個登陸臺風個例，分析了不同發展階段臺風大氣邊界層暖區變化的特徵及其與強度變化的關系。
  10. But the air temperature change in chongqing karst region was complicated, not only occuring warming region, but also colding region

    但巖溶區氣溫變化很復雜，既有變暖區又存在變冷區。
  11. At the same time, the effects of dragging force from fall of hydrometeors and latent - heat release from phase transfer are tested. from the analyses we conclude that the distributing of the cloud particles relates with temperature closely. huanan heavy rainfall and mei - yu front heavy rainfall have mixed - phase process with vapor phase, liquid phase and ice phase

    詳細分析了形成降水的雲物理過程，探討了源匯項對水凝物的貢獻，並通過敏感性試驗，考察了雲物理過程對降水熱力動力過程的反饋作用，研究結果表明：華南暖區暴雨和長江梅雨鋒暴雨的雲物理過程具有汽、水、冰三相混合雲特徵。
  12. 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 。
  13. The temperature of potential instability area was about 0 in the warm area and between - 10 and 0 in the cold area

    暖區位勢不穩定區位於0高度上下，冷區位勢不穩定區位於- 10 0高度之間。
  14. 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。
  15. 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。
  16. Positive vertical velocity existed between 700hpa and 500hpa

    暖區700 500hpa之間一般存在上升氣流。
  17. " the warm zones are spreading in this region into areas that weren ' t warm before

    溫暖區域正向在這個地區的非暖區擴大。
  18. The institute concentrates on the study of forming mechanism, physical process, forecasting technology of mesoscale heavy rain especially jianghuai meiyu front rain gush or heavy rain in prefrontal warmer area

    研究重點是我國陸地暴雨，特別是江淮梅雨鋒暴雨和鋒前暖區暴雨，同時開展我國北方暴雨的比較研究。
  19. The region getting warm appeared in the northeast of chongqing, the characteristics of which was that maximum air temperature became warmer than minimum air temperature. the regions getting cold took place in the middle and southeast of chongqing, mainly resulting from maximum air temperature

    變暖區發生在渝東北的巖溶區，主要特徵是最高、最低氣溫都變暖，但最高氣溫變暖幅度更大，變冷區在渝中和渝東南的巖溶區，主要是由最高氣溫的變冷造成的。
  20. 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。
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