陸面蒸發 的英文怎麼說

中文拼音 [liùmiànzhēng]
陸面蒸發 英文
evaporation of land
  • : 陸數詞(六的大寫) six (used for the numeral 六 on cheques, etc. to avoid mistakes or alterations)
  • : Ⅰ名詞1 (頭的前部; 臉) face 2 (物體的表面) surface; top 3 (外露的一層或正面) outside; the ri...
  • : Ⅰ動詞1. (蒸發) evaporate2. (利用水蒸氣的熱力使食物熟或熱) steam Ⅱ名詞[中醫] (將藥物隔水蒸熟) steaming
  • : 名詞(頭發) hair
  • 蒸發 : [物理學] [化學] evaporation; evaporate蒸發計 evaporometer; evaporimeter; atmidometer; atmometer; ...
  1. A simple two - component structure model for daily evapotranspiration

    散量計算的兩層阻抗遙感模型
  2. The hydrological cycle involves the movement of water in three phases from the ocean, land or living matter into the atmosphere by evaporation and transpiration and back into the earth s surface through a chain of complex atmospheric processes

    水以三種不同的型態水汽液態水冰,自洋麵地及動植物透過騰進入大氣層,又通過一連串復雜的大氣過程返回地球表。整個循環稱為水分循環。
  3. However, to hydrological cycle which contains the processes of preciptation, run - off, evaporation and storage of soil water, the heterogeneity of physical and ecological characteristics of soil surface and their description method and the hydrologic flux to land surface is still a challengeable problem in modeling of land surface

    然而,對于包括降水、徑流、,土壤層儲水等環節在內的整個水分循環過程來說,地表物理和生態特徵的非均勻性及其描述方法和水文通量參數化問題,迄今仍然是困擾過程模擬的挑戰性難題之一。
  4. The alternative changes of paleoenvironment favored the formation and imbedding of brine, which is the source of salt - water intrusion ; and the paleochannel that formed during regressive of sea level is the path of salt - water intrusion

    海進時期,大積的濱海平原被淹沒,在近海平原窪地滯留的海水經過、濃縮變為鹵水,成為鹹水入侵的物源;海退後源碎屑在濱海地區沉積形成了巨厚的古河道砂層。
  5. In this paper, starting with the physical mechanics of land surface hydrologic process and the introduction of the theory in probability statistic distribution, an analytical expression of heterogeneous evapotranspiration efficiency is given which takes heterogeneous soil water content ' s subgrid scale spatial variability into account, through which the parameterization scheme of subgrid scale soil surface ' s evapotranspiration efficiency ( which is generally called mosaic method ) is modified to a statistic - dynamic scheme in which a whole heterogeneity of the grid region is considered

    本文從水文過程的物理機制出,引進概率統計分佈理論,推導出一種由非均勻土壤含水量次網格尺度空間變率所形成的非均勻散率解析表達式,從而將通常的次網格尺度地表散率的參數化方案( mosaic方法) ,改進為考慮網格區整體非均勻性的統計-動力參數化方案。
  6. Sometimes called global dimming, the reduction in solar radiation varies from region to region, and no measurements have yet been made over the world ' s oceans

    有時也被稱為全球漸暗的日光減弱現象,在不同地區地上的程度並不一致,而且至今也沒有任何海上的測量資料,只是此一現象是可以由全球的率資料推導出來。
  7. There are 3 distribution types : i. e. whole district is the same, north and south part difference, and east and west part difference

    陸面蒸發呈增加趨勢,全區變化較為一致,中心在華北地區中部的濟南、臨沂一帶。
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