shortwave radiation 中文意思是什麼

shortwave radiation 解釋
短波輻射
  • shortwave : n. 短波;短波無線電發射機。2. vt. 用短波無線電發射[播送]。
  • 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. 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:地表特徵參數(植被指數ndvi 、地表反射率、地表溫度) ;地表輻射平衡各量(地表短波吸收輻射、地表長波輻射、大氣逆輻射、地表凈輻射) ;地表熱量平衡各量(土壤熱通量、顯熱通量、潛熱通量) 。
  2. The regression equation to estimate the cloud shortwave radiative forcing was established, the result can be used to estimate the cloud shortwave radiation forcing, thus remedying the shortage of radiation data. the surface global radiative flux which occurs for clear skies was computed by using modtran3 model and sounding data and that which actually occurs with cloudiness was from the routine data

    利用中解析度輻射計算模式modtran3和站點的探空資料以及地面資料,計算出無雲情況下的地面總輻射,再與實際情況下的實測地面總輻射結合得出雲對太陽輻射的強迫,分析了短波雲輻射強迫和實測地面凈輻射的關系。
  3. The characteristics of the annual period of absorbing shortwave radiation on sea surface are remarkable in nansha and xisha, with the maximum appearing in the winter - half year

    南沙和西沙海面吸收短波輻射年周期特徵明顯,極大值出現在冬半年。
  4. Through the analysis on the effects from the different aspects in the equal elevation grids upon the solar shortwave radiation received by ground surface, it is indicated that the discrepancy of landform elements leads to redistribution of the heat and cold sources of the ground surface and affects the snowmelt runoff, and then the aspect estimation is also taken as an important input to be inset into the model calculation

    通過分析同一高程網格坡向不同及其對到達地面太陽短波輻射通量的影響,提出地形要素差異導致地面冷熱源再分佈,調控融雪出流量,繼而將坡向判斷也作為系統重要輸入項之一嵌入到模型計算中。
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