凈輻射表 的英文怎麼說

中文拼音 [jìngshèbiǎo]
凈輻射表 英文
net radiometer
  • : Ⅰ形容詞1 (清潔; 干凈) clean 2 (凈盡;沒有剩餘) empty; hollow; bare 3 (純) net Ⅱ動詞(使干凈;...
  • : 名詞(車輪中車轂和輪圈的連接物) spoke
  • : Ⅰ動詞1 (用推力或彈力送出) shoot; fire 2 (液體受到壓力迅速擠出) discharge in a jet 3 (放出) ...
  • : Ⅰ名詞1 (外面;外表) outside; surface; external 2 (中表親戚) the relationship between the child...
  • 輻射 : radiation; exposure; radio; beaming
  1. The results showed that the evapotranspiration calculated by bowen ratio was highly related to solar radiation, but that calculated by lysimeter was not evidently related to solar radiation

    結果明,波文比所測蒸發蒸騰量與太陽的相關性比較好,蒸滲儀所測值與太陽的相關性不明顯。
  2. Moreover, evapotranspiration consumes mainly net radiation on a clear day and sensible heat flux is greater than latent heat flux on a cloudy day above spring wheat field

    在有植被覆蓋或裸地下墊面,晴天、陰天的、潛熱、感熱及土壤熱通量均現出了與平均狀況一樣的日變化特徵。
  3. ( 2 ) based on gaining the surface parameters, to compare to diversified retrieve model to choose optimal one to retrieve net radiance flux, soil heat flux and latent heat flux, which settle the groundwork to calculate the regional et

    在獲取地參數的基礎上,反復對比前人各種遙感反演模型,選擇最佳模型對長江三角洲的區域通量、土壤熱通量、潛熱通量進行了反演,為計算區域蒸散量奠定了基礎。
  4. The previous methods to parameterize instantaneous clear - sky surface total radiation and net radiation is discussed

    摘要討論了晴天地太陽總和地太陽瞬時值的參數化方法。
  5. Similarly, the net radiation on a cloudy day is mainly used up evaporation of soil. the integrated value of soil heat flux is negative on a cloudy day and that shows the soil emits the heat, which is different on a clear day. in short, average latent, sensible and soil heat flux is 67 %, 21 % and 6 % of net radiation respectively

    在裸地下墊面時,晴天潛熱佔到的60 ,顯熱交換只佔到19 ,在陰天同樣主要消耗于土壤蒸發,與晴天不同的是在陰天土壤熱通量積分值小於零,明土壤在向外釋放熱量;平均狀況下,潛熱、顯熱和土壤熱通分別佔到的67 、 21和6 。
  6. After analyzing the equations, we find the standard error of them is less distinction and adapt to different circumstance. we test the model over jinan area and find the model is available. by using the visible and infrared picture at 14, on july 1, 1994, the model can help us know the distribution situation over certain area

    以濟南地區和1994年7月1日14時的紅外和可見光數字雲圖資料兩個個例作了檢驗,結果明用衛星數字雲圖資料反演08 - 17時各時刻地通量是可行的,並且可以了解一定區域內地的分佈狀況。
  7. 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時總地與衛星紅外和可見光數字雲圖反演的能量的關系,研究明08 - 17時總地與衛星可見光反演得到的地氣系統反的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時總地與地氣系統發的紅外相關顯著。
  8. The results show that a warm high ridge at the middle level and transformed surface cold high over the plain provide a good background condition ; a cooling process produced by net surface radiation fluxes is the trigger and strengthening mechanism for the fog event ; the subsidence flow at the middle and low tropospheric levels is favorable for the setting - up and maintenance of stable stratification at the boundary layer and weak wind condition at the ground layer over the fog region ; the transportation of weak warm advection at lower levels and weak lift motion at the boundary layer play a very important role to the long maintenance of the fog event ; the intrusion of north wind accompanied by cold advection is a main dynamic factor of the fog dissipation

    結果明:在中高層暖性高壓脊及地面變性冷高壓穩定維持的大尺度背景條件下,地引起的近地層冷卻是大霧過程的觸發和加強機制;中低空下沉氣流的存在有助於近地層的弱風條件和穩定層結的建立;低層暖平流的輸入和邊界層的淺層抬升是大霧長時間持續的原因;伴隨冷空氣南下的偏北大風是驅使大霧消散的動力因子。
  9. 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,根據地能量平衡方程,通過計算對地反照率、地溫度、地系數、歸一化植被指數等參數進行反演,進一步計算出了地通量,土壤熱通量和潛熱通量,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。
  10. 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紅外,可見光雲圖反演出地氣系統反的太陽,然後採用多元統計的方法討論了地與衛星反演出的值之間的關系。
  11. ( 3 ) compared with bare soil, income of net radiation declined, apparent heat weakened and latent heat exchange were almost disappeared on the soil surface with film

    ( 3 )薄膜覆蓋于土壤面后,與未覆蓋的土壤相比,地r _ n收入下降,顯熱交換p減弱,潛熱交換le趨于零。
  12. It is found in this paper that : 1. the radiation computing solution developed by zhou suoquan et al. shows good performance on the fluxes simulation of the total surface radiation and net surface radiation, which can reflect the annual and daily radiation change very well, and radiation differences between clear day and cloudy day as well

    結果明: 1 )該計算方案對于漠河總通量和通量有較好的模擬性能,能夠較好地模擬出通量的年變化和日變化的特點,對于晴天和雲雨天氣通量的差別也能較好地模擬出來。
  13. Some variables regional distribution over south ningxia is given out in the course of evapotranspiration estimation : the regional distribution of surface characteristic parameters ( normalzed difference vegetation index, surface albedo, surface temperature ), radiation balance components ( surface absorbed shortwave radiation, surface longwave radiation, atmospheric counter radiation, net radiation ), surface heat and balance components ( soil heat flux, sensible heat flux, latent heat flux )

    估算區域蒸發(散)量的過程中,得到許多有意義的量:地特徵參數(植被指數ndvi 、地率、地溫度) ;地平衡各量(地短波吸收、地長波、大氣逆、地) ;地熱量平衡各量(土壤熱通量、顯熱通量、潛熱通量) 。
  14. Roughly acquire optical depth of clear sky and clouds from radiation station data and routine meteorological data of land surface, and the study the relationship between clouds " physical character and radiation. obtain the relationship between surface and near - ground atmosphere, and then according to this estimate surface albedo and surface net. by analyzing the relationship between satellite visible spectra, infrared spectra, and water vapor spectra values and radiation, by means of radiation transfer theory, analyze and deducethe relationship between clouds and radiation, and establish relationships between satellite value and global radiation and net

    通過衛星雲圖的計數值來判斷雲對的作用,以此建立起它們之間的關系;利用地面觀測資料和常規資料來粗略求取晴空大氣和雲光學厚度,進而研究雲的物理屬性與關系;簡單的獲取地與近地面大氣之間的關系,以此估算地的反照率,和地;分析了衛星可見光、紅外及水汽雲圖計數值和地面之間關系,利用傳輸公式來推倒和分析雲對的關系,試圖建立起衛星測值與地之間的關系,並將晴空和有雲的個例分開,分別建立並選出最佳模式,以此來估算地和總
  15. 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明不同時間間隔的邊界強迫對地吸收的短波和釋放的潛熱影響較大。
  16. The results show that loss of hydraulic conductivity of robinia xylem embolism is different under the condition of different soil humidity and loss of hydraulic conductivity is related with net photosynthetic rate, transpiration rate, stomatal conductance, the flow of water, atmospheric temperature, relative humidity, photosynthetic available radiation, and hydraulic conductivity

    研究結果明:木質部導水率損失在不同的土壤含水量以及不同的測定時間條件下是有顯著性差異的;刺槐的導水率損失與光合速率、氣孔導度、水勢、蒸騰速率、光合有效、大氣溫度顯著相關。
  17. 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對地域的敏感性。
  18. 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

    結果明08 - 17時地通量與大氣頂太陽、地氣系統發紅外和地氣系統反的太陽線性相關,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時各時刻地通量的估算模式(適用於各種天氣情況) 。
  19. The research of surface net radiation is vital to weather, climate, entironment, ocean, etc. as yet the work of this field in our country is few

    的研究對于天氣、氣候、環境、生態、水利、海洋等領域具有重要研究價值,目前這方面的研究並不多見。
  20. 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

    然後將地率的影響作為誤差項進行訂正,從而得到各種地率條件下的晴天地太陽的計算方法。
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