熱帶東風帶 的英文怎麼說

中文拼音 [rèdàidōngfēngdài]
熱帶東風帶 英文
subtropical easterlies
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  • 熱帶 : tropics; burning zone; [氣象學] torrid zone熱帶草原 campos; llanos savanna; [巴西] matto grosso; ...
  • 風帶 : airhose
  1. Tropical storm emily closed in on the windward islands of the eastern caribbean on wednesday, prompting storm warnings from barbados to the netherlands antilles

    熱帶風暴艾米麗emily星期三在東加勒比海的上風小島登陸，巴貝多島迅速向荷蘭安的列斯群島發出警告。
  2. Jiangsu province lies in the east of china and is in the downriver area of the changjiang river and the huaihe river

    江蘇省位於我國大陸東部，地處長江、淮河下游，在亞熱帶季風氣候的影響下，是我國自然災害出現較多的省份之一。
  3. ( 4 ) summer rainfall anomalies in north china relates to the indian summer monsoon, the south sea monsoon, sub - tropical anticyclone, south asian anticyclone and cold air anomaly

    （ 4 ）華北地區夏季降水異常與印度西南季風、南海東南季風、副熱帶高壓、南亞高壓及冷空氣異常都密切相關。
  4. ( 5 ) there exists close relationship between the meiyu period precipitation in jianghuai valleys and the anomalies of subtropical summer monsoon, the anomalies of cold air, not the same so the indian summer monsoon

    （ 5 ）江淮地區梅雨期降水與東亞副熱帶季風、北方冷空氣異常密切相關，與印度西南季風關系並不密切。
  5. Zhoushan has a northern subtropical monsoon marine climate with clear four seasons ; leading wind directions are southeast wind in summer, northwest wind in winter. with an annual average wind speed of 3. 3m s ; and an average temperature of 15. 6 - 16. 6, and the frost free period reaches 251 - 303 days perannum, annual average sunshine time 1941 - 2257 hours, and the annual preeipitation is 927 - 1620 mm

    舟山屬北亞熱帶南緣季風海洋型氣候，四季分明主導風向，夏季為東南風，冬季為西北風，年平均風速3 . 3米秒年平均氣溫15 . 6 . - 16 . 6 ，冬季最低溫為- 1 ，夏季最高溫度為37無霜期251 - 303天，年日照時數1941 - 2257小時年降雨
  6. During the el nino ( la nina ) events, the negative ( positive ) sst anomaly occurs and the corresponding the olr mjo intensity weakens ( enhances ) in the tropical western pacific ; at the same time, the positive ( negative ) surface westerly anomaly leads to positive ( negative ) mld anomaly, and the corresponding sst mjo intensity weakens ( enhances ) in the equatorial eastern pacific, 4 ) the interdecadal variation of the atmospheric mjo intensity took place distinctly in 1970s in the tropical western, northwest and eastern pacific, with the stronger intensity in the former than the back stage, and the interdacadal variation of sst is its cause

    Elnino （ lanina ）事件中熱帶兩太平洋sst出現負（正）異常， olr季內振蕩強度出現減弱（增強）的變化。 elnino （ lanina ）事件中，赤道太平洋出現地面信風西風分量正（負）異常，並引起熱帶東太平洋mld出現正（負）異常，造成熱帶東太平洋sst季內振蕩強度出現減弱（增強）的變化。 4 ）熱帶印度洋、熱帶西太平洋和熱帶東太平洋季內振蕩強度在上世紀70年代發生了明顯的年代際變化，均為前弱、后強， sst本身的年代際變化是其原因。
  7. ( 4 ) there exist close relation between the floods season precipitation in northeast china and the anomalies of subtropical summer monsoon, the anomalies of cold air, sub - tropical anticyclone, polar front jet, north hemisphere general circulation anomalies in winter

    （ 4 ）東北汛期降水與西南夏季風、北方冷空氣、副熱帶高壓、極鋒急流、前期冬季環流異常密切相關。
  8. 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。
  9. ( 3 ) the polar eddy, the west circumfluence on 500hpa medium latitudinal region ands subtropic circumfluence are the key systems of tpnes floods precipitation and, the wet years have abundant vapor, moreover, the omga is positive in all atmosphere

    （ 3 ）極渦、中高緯西風環流系統和副熱帶系統是影響青藏高原東北側區汛期降水的大尺度環流背景關鍵系統。同時，多雨年的主要流場特點是有利於水汽輸送，且整層大氣始終表現為上升運動。
  10. ( 2 ) sxsp anomaly is closely related to the abnormity of 500hpa geopotential height field over the east of ural and yakutsk area, western ridge point and area of subtropical high, the cold air abnormity from north of china and the position of upper level westerly jet over east asia

    （ 2 ）三峽庫區夏季降水異常與大氣環流異常密切相關：與500hpa烏拉爾山以東高度場異常、雅庫茨克以東高度場異常、副熱帶高壓面積及西伸脊點、北方冷空氣異常、 200hpa東亞高空西風急流位置異常偏南（偏北）密切相關。
  11. If a decadal positive temperature anomaly occurs in the eastern tropical pacific, the atmospheric response excites a anticyclonic wind stress anomaly in the east of australia, which will lead to generate a negative temperature anomaly in the western tropical south pacific

    當熱帶東太平洋的海溫為暖異常，它將激發澳大利亞的東部沿岸的大氣產生反氣旋性風應力異常，在這種風場的作用，下方海水向四周輻散，導致熱帶西南太平洋的溫躍層變淺，產生負的溫度異常。
  12. According to main weather types, this paper determines the criterion for choosing typical month of meteorological model used in buildings energy efficiency, and founds the procedures of annual meteorological model in hot summer and warm winter zone

    本文以深圳市為例，研究夏熱冬暖地區建築師用建築能耗計算方法。深圳市地處東南沿海，屬亞熱帶季風海洋性氣候，是夏熱冬暖地區的典型。
  13. The analysis of the large - scale synoptic situation shows that strong precipitation is closely related to the explosion of monsoon and the intensification of cross - equatorial flow which bring a lot of vapor and meet with cold masses at the eastern of northwest district on 8th, june causing extremely heavy rainfall ; that subtropical high - level jet at 200hpa, subtropical high at 500hpa and low - level jet at 850hpa are the weather backgrounds favorable to strong precipitation ; that the pattern of eastern highs and western lows and the establishment of a low - level jet and the coupling between upper - and low - level patterns that determine that the rain occurred in the east of the northwest china ( on average, this is the rainy season for the south of china, but not for the northwest china ) ; that water vapor comes from southerly and easterly flow which converge at the eastern of northwest district with convergence mainly in lower levels and pbl ; that the high value of the whole - level apparent heat source < q1 > is near the area of large rainfall in the direction of northeasterly - southwesterly agreeable to shear line very well and the condensation latent heat releasing is main heat source with vertical advection item playing key role in q1 and q2 ; that there is a vertical secondary circulation crossing low - lever jet whose ascending branch is at the area of large rainfall ; that the construction of convection instability and conditional symmetry instability results that there is not only deep thermal instability, but also moisture influx and triggering mechanism of thermal instability causing strong torrential rain

    作為對比，本文還對2002年6月24 - 25日發生在北京地區的強地形雨進行了分析，並討論陜南、北京地區兩地暴雨的異同點以及地形作用的共性和個性，為兩地暴雨預報提供有益的參考，得出了一些很有意義的結果： 1大尺度環流背景分析表明： （ 1 ） 「 02 . 6 」強降水與6月上旬越赤道氣流和季風爆發密切相關，攜帶大量水汽的偏南氣流與冷空氣於6月8日交匯在西北地區東部，導致了這次強降水的發生； （ 2 ） 200hpa的副熱帶西風急流、 500hpa副高以及850hpa的低空急流的配置非常有利於本文分析之陜西強降水的發展與維持。大尺度形勢分析表明，東高西低形勢場、低空急流的建立和高低空形勢的配置決定了這場降雨出現在西北地區東部。與暴雨區相聯系，存在一支橫越低空急流的經向垂直環流，暴雨區處于該垂直環流的上升支； （ 3 ）偏南和偏東氣流水汽通道在西北地區東部交匯，水汽的輻合積聚主要在對流層低層和行星邊界層內完成； （ 4 ）整層的視熱源< q _ 1 >高值區在暴雨區附近呈東北-西南向分佈，與切變線走向非常一致，降水產生的凝結潛熱釋放是強降水區大氣的主要熱源。
  14. Seasonal variations of water vapor transport over east asia monsoon region are studied, especially that in summer season. the results indicate that there are four vapor inflow corridors to fetch china : southwest corridor, south china sea corridor, southeast corridor and northwest corridor. it shows impact of south asia monsoon, south china sea monsoon, subtropical monsoon and middle latitude westerly belt on summer rainfall anomaly over china, respectively

    分析了東亞季風區水汽輸送的季節變化，並著重研究了夏季東亞季風區的水汽輸送特徵，指出夏季東亞季風區水汽輸送有四條通道到達中國大陸：西南通道、南海通道、東南通道和西北通道，分別體現了南亞季風、南海季風、副熱帶季風和中緯度西風帶對中國夏季降水的影響。
  15. Dengue fever is endemic in many subtropical and tropical areas, especially in southeast asia and latin america

    登革熱是亞熱帶及熱帶地區的風土病，在東南亞及拉丁美洲特別流行。
  16. When the heat source over philippines is abnormally weak, the southern asian high becomes only one part and its location extends southward, the indian summer monsoon is stronger, the eastern asian tropical summer monsoon is weaker, and the western pacific subtropical high extends southward ; the influence of the heat source strong anomalies over philippines on the east part of the southern asian high and the western pacific subtropical high and the east asian tropical summer monsoon is significant and whic h on the indian summer monsoon is not significant ; the influence of the heat source weak anomalies over philippines on the east asian tropical summer monsoon and the indian summer monsoon and the western pacific subtropical high and the southern asian high is significant

    東亞熱帶季風加強，南亞季風也有所加強，西太平洋副熱帶高壓位置偏北；當夏季菲律賓熱源異常減弱時，南亞高壓只表現為一個部分，且位置偏南，南亞季風加強，東亞熱帶季風減弱，西太平洋副熱帶高壓位置偏南。夏季菲律賓熱源異常強年，東部的南亞高壓異常顯著，副熱帶高壓位置異常偏北也達到顯著水平，東亞熱帶季風的加強是顯著的，而南亞季風的加強並不顯著；而熱源異常減弱時，東亞熱帶季風的減弱、南亞季風的加強都達到顯著水平，副熱帶高壓、南亞高壓的位置異常偏南也是顯著的。
  17. 6 ) the correlation relationships of the mjo of daily 10m - wind ( v ) fields with that of sst fields are investigated by time - lagged svd method in the north pacific, south pacific and the tropical eastern pacific, and the basal process of v and sst mjo obtained in the three areas, which is a negative feedback process drived by drift and sensible heat under the conditions of shallow mld, is probably the maintaining mechanism

    6 ）用時滯svd方法分析了北太平洋、南太平洋、熱帶東太平洋區域10米高處逐日風（夕）場與sst場季內振蕩的相關聯系，得到了三區夕、 sst場季內振蕩的基本過程，它們是由漂流和感熱輸送推動的一個負反饋過程，它以薄mld為存在條件，可能是sst季內振蕩的維持機制。
  18. Mianyang city belongs to eastern subtropics monsoon climate region, moderate climate, and distinctive four seasons

    綿陽市境內屬于東部亞熱帶季風氣候區，氣候溫和，四季分明。
  19. " residents of onslow are warned that very destructive winds will soon resume without warning from a different direction, " australia ' s bureau of meteorology said in its latest cyclone warning " very destructive gusts to 235 kmh are expected near the cyclone center, and are occurring on the coast in the vicinity of onslow, " it said

    當地搶險部門預計，此次熱帶氣旋帶來的危害有可能接近10天前橫掃澳大利亞東北部的氣旋「拉里」以及去年8月給美國新奧爾良地區帶來重大損失的「卡特里娜」颶風。
  20. " residents of onslow are warned that very destructive winds will soon resume without warning from a different direction, " australia ' s bureau of meteorology said in its latest cyclone warning www. bom. gov. au. " very destructive gusts to 235 kmh are expected near the cyclone center, and are occurring on the coast in the vicinity of onslow, " it said

    當地搶險部門預計，此次熱帶氣旋帶來的危害有可能接近10天前橫掃澳大利亞東北部的氣旋「拉里」以及去年8月給美國新奧爾良地區帶來重大損失的「卡特里娜」颶風。
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