net solar radiation 中文意思是什麼

net solar radiation 解釋
凈太陽輻射
  • net : n 因特網。 supply Net services 提供因特網服務。 n 1 網,網眼織物,(花邊的)織物。2 網狀物,網狀...
  • solar : adj 太陽的,根據太陽運行測量的;因太陽作用產生的。n = solarium the solar system 太陽系。 a solar...
  • radiation : n. 1. 發光,射光,放熱,放射,發射。2. 【物理學】輻射;放射物;輻射線[熱、能];照射(作用)。3. 【動、植】輻射形;【測】射出測量法;【醫學】射線療法。
  1. Radiative forcing is defined as a change in average net radiation at the top of the troposphere tropopause due to a change in either solar or infrared radiation

    輻射力的定義是由於太陽或紅外線輻射份量的轉變而引致對流層頂部的平均輻射改變。
  2. Radiative forcing is defined as a change in average net radiation at the top of the troposphere ( tropopause ) due to a change in either solar or infrared radiation

    輻射力的定義是由於太陽或紅外線輻射份量的轉變而引致對流層頂部的平均輻射改變。
  3. In this paper we also discuss the relationship between the total net radiation from 08 to 17 and the total solar radiation retrieved from the satellite visible picture at the same time interval. the result reveal the total surface net radiation is evidently reverse to the total solar radiation, the correlation coefficient of one station is high to 0. 9. but tianjin is exceptional, the total surface net radiation is correlative to the total infrared radiation

    同時探討了08 - 17時總地表凈輻射與衛星紅外和可見光數字雲圖反演的輻射能量的關系,研究表明08 - 17時總地表凈輻射與衛星可見光反演得到的地氣系統反射的08 - 17時各時刻的和反相關顯著,個別站點相關系數達0 . 9以上,但也有一例外,天津站08 - 17時總地表凈輻射與地氣系統發射的紅外輻射相關顯著。
  4. The simulations of ground temperature and earth absorbed net solar radiation are lower than the observation. sensible heat and latent heat are also lower than the observation

    由於模式模擬的地溫偏低,凈的短波輻射偏小,則模擬的感熱和潛熱值偏小。
  5. The infrared radiative fluxes emitted by earth - atmosphere system comes from the infreared pictures and the solar radiative fluxes reflected by earth - atmosphere system comes from the visible pictures, then the relationship between the surface net radiation and the satellite retrieval radiation is statistically discussed in this paper

    由紅外雲圖反演出地氣系統發射紅外輻射,可見光雲圖反演出地氣系統反射的太陽輻射,然後採用多元統計的方法討論了地表凈輻射與衛星反演出的輻射值之間的關系。
  6. The results show time interval of atmospheric forcing gives rise to significant difference in net solar radiation and latent heat in siberia area

    西伯利亞地區的單點試驗表明不同時間間隔的邊界強迫對地表吸收的凈短波輻射和釋放的潛熱影響較大。
  7. The paper test the model over jinan and nanjing, and reveal the sensitivity of the total net radiation to the total solar radiation reflected by earth - atmosphere system

    同時採用濟南和南京作了檢驗並說明估算地表凈輻射對地域的敏感性。
  8. The result show that the surface net radiative fluxes is linear to the solar radiation of top of atmosphere, the infrared radiative fluxes emitted by earth - atmosphere system and the solar radiative fluxes reflected by earth - atmosphere system. the correlation coefficient keep on a high level. and in this paper we develop the regression equations ( for all days and for cloud days ) to estimate the surface net radiation on an hour scale

    結果表明08 - 17時地表凈輻射通量與大氣頂太陽輻射、地氣系統發射紅外輻射和地氣系統反射的太陽輻射線性相關,相關系數維持在一個較高值,並建立了用衛星資料反演08 - 17時各時刻地表凈輻射通量的估算模式(適用於各種天氣情況) 。
  9. The net surface solar radiation ( nssr ) as one of the most important portion of global radiation budget has a great action to solar energy absorbed by surface and then affect the surface radiation budget and atmospheric dynamical process

    其中地表凈太陽輻射的衛星遙感是全球輻射平衡遙感中的一個重要部分,因為它代表了地表吸收的太陽輻射能量,對地表輻射平衡和大氣動力過程等有著重要的作用。
  10. The global distribution of nssr can be provided by means of satellite remote sensing. in this paper a new parameterization derived by li zhan - qing ( li model ) in 1995 was used to compute the net surface solar radiation for 18 stations of chinese main land on some days over january and february in 2001. after compared the results of li model with those derived from a model ( li - leighton model ) and b model ( langley parameter model ) for clear - sky and cloud - sky respectively, we founded that the relative difference of the two model are below 6 %

    結果表明:在晴天情況下, li模式與a模式很相近,而與b模式結果差別較大,因為b模式在晴空條件下是不準確的,這也可以從a模式與b模式的差別看出;在雲天情況下, li模式與b模式結果盡管有些差異,但是相似性仍然很好,除了個別的臺站外,絕大部分臺站兩者的相對差在6以內。
  11. The parameterization of clear - sky surface solar net radiation under the conditions of various albedos is obtained through the error correction due to albedo variation

    然後將地表反射率的影響作為誤差項進行訂正,從而得到各種地表反射率條件下的晴天地表太陽凈輻射的計算方法。
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