熱反照率 的英文怎麼說

中文拼音 [fǎnzhào]
熱反照率 英文
bolometric albedo
  • : Ⅰ名詞1 (方向相背) reverse side 2 (造反) rebellion 3 (指反革命、反動派) counterrevolutionari...
  • : Ⅰ動詞1 (照射) illuminate; light up; shine 2 (反映) reflect; mirror 3 (拍攝) take a picture ...
  • : 率名詞(比值) rate; ratio; proportion
  1. A transfer model is established, which can be used to study the interaction between the land surface physical processes of inhomogeneous region and the structure of atmosphere boundary - layer over urban and rural terrains. the model has simulated surface heat flux, surface temperature, temperature profiles, height of mixture layer and so on. and the differences between urban area, suburban area and rural area have been compared. this model mainly depends on the parameters below : surface albedo, surface roughness coefficient, moisture available coefficient of soil, thermal capacity and thermal diffusion coefficient of errain, cloudage. the result shows that this model can simulate the structure and eigenvalues of atmosphere boundary layer and their changes in a day. parameters used in this model aim at beijing city, and the time is at the beginning of september. to other cities, or other time, the parameters should be adjusted accordingly. in addition, being adjusted, the model can also be used for other homogeneous and inhomogeneous terrains

    模式主要依賴于以下參數和物理量:地面下墊面粗糙度土壤的可含水量下墊面的容量和擴散系數雲量等參數。結果表明,本模式能合理地模擬不同地表量平衡地表氣溫混合層高度湍流交換系數湍流動能位溫廓線等,以及它們的日變化。該模式所取參數主要針對北京市,時間為九月初,對于其他城市,參數應作相應的調整。
  2. The objective of this paper is to retrieve the albedo of the plateau and then to calculate the parameters about hot or cold source quantitatively

    本文的目的是對青藏高原地表和冷源參數進行定量演。
  3. Then basing the empirical formal proposed by weng burning, a method for reckon the average flux of energy transfer from ground surface to the air of a day according albedo and terrain parameters was put forwarded. it is considered that the flux is a proper index to decide if the area is a hot source or a cold source

    然後,在翁篤鳴等提出的有關半經驗公式的基礎上,提出了根據和地形參數計算高原地面向大氣輸送能量的日平均通量的演算法,並以此作為判定冷源的標準。
  4. This study dealt with the identification and evaluation of 8 maize populations from tropical and subtropical regions under the ecological conditions in zhengzhou, henan. results showed that the significant delaying days to shed and days to silk, discoordinating for the development of male and female, higher plant and ear height, more leaf numbers, high barreness, worse performance of ear traits compared with the ck ( temperate population ) were found, which showed the tropical and subtropical populations could not be utilized directly under the ecological conditions in zhengzhou. by using selection and improvement the tropical and subtropical populations can be used to broaden the genetic base of temperate maize breeding, beause of the greater genetic variation and higher selection potential within each population. the different performances of the sensitivity to photoperiod were observed among different tropical and subtropical populations and different traits. the asi, time to silk, ear height, leaf numbers, grain yield per ear could be used as the good evaluation traits for identifying the sensitivity to photoperiod

    對8個帶、亞帶玉米群體在鄭州生態條件下的表現進行鑒定和評價,結果表明,帶、亞帶群體散粉、吐絲期顯著延遲,雌雄不協調,植株和穗位高、葉片數增多、空稈高,結實性差,果穗性狀均明顯劣於溫帶對,在鄭州生態條件下不能直接利用,但是群體內具有較大的遺傳變異和選擇潛力,可以用來拓寬現有玉米種質的遺傳基礎;不同帶、亞帶群體的光周期敏感性不同;不同性狀對光周期應的敏感程度不同, asi 、吐絲期、穗位高、葉片數、穗粒重可作為鑒定光周期敏感性的較好指標
  5. In short, through retrieving the parameter such as surface albedo, surface temperature and surface emissivity, all the energy flux such as net radiance flux, soil heat flux and latent heat flux can be computed in sequence further, then latent heat flux which provide energy for et can be computed based on energy balance equation, finally instantaneous et and daily et can be obtained

    總之,根據地表能量平衡方程,通過計算對地表、地表溫度、地表比輻射系數、歸一化植被指數等參數進行演,進一步計算出了地表凈輻射通量,土壤通量和潛通量,最後獲得了遙感影像成像時的瞬時蒸散及當天的總蒸散量。
  6. The simulated latent heat of coarse soil is smaller, and surface temperature and sensible heat is larger than the results of the control run

    粗糙土壤,大,造成地面吸收短波輻射減少。粗糙土壤用於蒸發的潛減少,地溫升高,感大。
  7. The fine soil characters have little variation of albedo and absorbed solar radiation. the simulated sensible heat is lower than the result of the control run in clay case

    粘土變化不大,因此吸收太陽輻射變化不明顯,用於蒸發的潛變化不明顯,地溫略降低,感變小。
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