warm area 中文意思是什麼

warm area 解釋
溫區
  • warm : adj 1 暖和的，溫暖的；保暖的。2 熱情的，熱心的，熱烈的；多情的。3 易怒的；興奮的；激烈的，激昂的...
  • area : n. 1. 面積；平地；地面。2. 空地；〈英國〉地下室前的空地。3. 地區，地方；〈比喻〉區域；范圍。
  1. A front is a transition area between the cold and warm air masses

    鋒或鋒面是指冷暖氣團之間的過度帶。
  2. 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。
  3. A sea - breeze front was clearly discernible over an area on the western part of the airport where outgoing winds the background wind, warm colours and incoming winds sea breeze, cold colours met

    清楚的顯示機場西面出現一道海風「鋒」 ，這正是遠離激光雷達的氣流背景風，暖色和趨向激光雷達的氣流海風，冷色相遇的位置。
  4. A sea - breeze front was clearly discernible over an area on the western part of the airport where outgoing winds ( the background wind, warm colours ) and incoming winds ( sea breeze, cold colours ) met. this new piece of equipment had enabled the observatory to issue in advance a windshear alert for that occasion

    清楚的顯示機場西面出現一道海風「鋒」 ，這正是遠離激光雷達的氣流背景風，暖色和趨向激光雷達的氣流海風，冷色相遇的位置。這套新的儀器令天文臺能夠于該天提早發出了風切變預警。
  5. A sea - breeze front was clearly discernible over an area on the western part of the airport where outgoing winds the background wind, warm colours and incoming winds sea breeze, cold colours met. this new piece of equipment had enabled the observatory to issue in advance a windshear alert for that occasion

    清楚的顯示機場西面出現一道海風「鋒」 ，這正是遠離激光雷達的氣流背景風，暖色和趨向激光雷達的氣流海風，冷色相遇的位置。這套新的儀器令天文臺能夠于該天提早發出了風切變預警。
  6. In the warm period, the aquatic bivalvia was well - developed, and the gastropod fauna was obviously prosperous and characteristic by large amount of the aquatic species. the alternative appearance of both cold and the warm mollascan assemblage tpyes reflects the features of the quaternary climate changes in this area

    在冷期因氣候乾燥，環境中水量減少，腹足類化石以陸生肺螺類最為發育；在暖期水生雙殼類較為發育，腹足類群明顯繁盛，以水生種類的大量出現為特徵。
  7. Guernsey is one of the channel islands in the southwest - central english channel. a guernsey is a warm, knitted wool shirt first worn by seaman in this area

    根西島是位於英吉利海峽西南靠中部的海峽島嶼之一。根西衫是一種暖和的針織羊毛衫，最初為該地區的水手穿著。
  8. And vibrant modern dance favored by young people amply demonstrated the jubilance and enthusiasm of these modern spiritual practitioners. the elegant publication corner, exhibition area for celestial clothes and jewelry, and children s amusement section all resounded with joyful laughter during the event as crowds filled the center with a warm and cheery atmosphere. next to the kitchen was the canteen area, where delicious vegetarian food was served to fellow practitioners and guests throughout the day

    舞臺上優美動人的歌聲饒富民族風味的舞蹈及年輕人的動感勁舞，充分展現了現代修行人活潑開朗及樂觀洋溢的一面會場並設有雅緻的經書區天衣天飾區和充滿歡樂的兒童游戲區，川流不息的人潮，帶動了整個道場熱鬧歡騰的氣氛，廚房旁邊的用餐區更是全天候為同修及來賓供應美味的素食佳肴。
  9. 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。
  10. It could play an important role in the evolution of " warm pool " area. more than 300 pure psychrophilic and psychro - tolerant bacteria were isolated from environmental samples

    對深海沉積物和極地環境樣品進行了低溫微生物的分離和培養，得到了300多株嗜（耐）冷細菌，並對其進行了生長特性的分析。
  11. 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。
  12. Members of the cfb ( cytophaga - flexibacter - bacteroides ) were found to be rich in upper sediment of " warm pool " while they were not detected in sediment from " manganese nodule " area, which indicated that there were more organic substances in the " warm pool " area

    除了紫細菌之外， cfb類群在「暖池」區沉積物中也是一類較重要的細菌，主要集中在表層沉積物；而在「結核」區沒有檢測到屬于cfb類群的細菌，表明「暖池」區表層存在較多的有機物。
  13. Caution : to avoid freeze damage to the test kit, it should be stored in a dry, warm area when not in use

    警告：為了避免冰凍對于檢測組件的破壞，在閑置時，應該把檢測組件存放在乾燥、溫暖的地方。
  14. 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 。
  15. 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。
  16. 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。
  17. 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。
  18. 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。
  19. Warm area 13

    十三溫區
  20. Warm area 14

    十四溫區
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