熱帶匯流區 的英文怎麼說

中文拼音 [dàihuìliú]
熱帶匯流區 英文
intertropical confluence zone
  • : Ⅰ動詞1 (匯合) converge 2 (聚集; 聚合) gather together 3 (通過郵電局、 銀行把款項劃撥到別處)...
  • : Ⅰ動1 (液體移動; 流動) flow 2 (移動不定) drift; move; wander 3 (流傳; 傳播) spread 4 (向壞...
  • : 區名詞(姓氏) a surname
  • 熱帶 : tropics; burning zone; [氣象學] torrid zone熱帶草原 campos; llanos savanna; [巴西] matto grosso; ...
  • 匯流 : (會合) converge; flow together; confluence; junction; sink flow匯流點 [地理學] confluence
  1. The yellow river delta that is one of three most largest estuary delta in china locates an intersect area between the economy circle around the bohai sea and the economy belt of the yellow river valley. natural resources like petroleum, natural gas, bittern and terrestrial heat enrich the yellow river delta area. moreover, the natural endow of wetland resources, marine products resources and land resources abound in this area

    黃河三角洲是我國三大河口三角洲之一,地處環渤海經濟圈和黃河域經濟的交點,有豐富的自然資源,如石油、天然氣、鹽鹵、地等,同時具有巨大的濕地資源、豐富的海產資源、廣闊的土地資源,土地利用變化劇烈,成為研究土地利用變化的點地之一。
  2. 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日發生在北京地的強地形雨進行了分析,並討論陜南、北京地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大尺度環背景分析表明: ( 1 ) 「 02 . 6 」強降水與6月上旬越赤道氣和季風爆發密切相關,攜大量水汽的偏南氣與冷空氣於6月8日交在西北地東部,導致了這次強降水的發生; ( 2 ) 200hpa的副西風急、 500hpa副高以及850hpa的低空急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東部。與暴雨相聯系,存在一支橫越低空急的經向垂直環,暴雨處于該垂直環的上升支; ( 3 )偏南和偏東氣水汽通道在西北地東部交,水汽的輻合積聚主要在對層低層和行星邊界層內完成; ( 4 )整層的視源< q _ 1 >高值在暴雨附近呈東北-西南向分佈,與切變線走向非常一致,降水產生的凝結潛釋放是強降水大氣的主要源。
  3. In drought or flood years over the yangtze river basin, the features of the establishment, progression and decrease of moisture transport is significantly different, meanwhile the differences of the moisture transport by the monsoon circulation between mid and low latitudes in the northern hemisphere, and by the subtropical high are obvious, so are their convergence, especially over south china sea, the tropical west pacific, the yangtze river basin, north china and north - east in china

    ( 4 )長江域旱澇年亞澳季風夏季風水汽輸送的建立、推進、減弱的階段性特徵顯著不同,對應的中低緯季風環、副高環等季風系統水汽輸送、合也有顯著差別,尤其是在南海、西太平洋、長江域、華北和東北等地
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