radiative forcing 中文意思是什麼

radiative forcing 解釋
輻射力
  • radiative : adj. 1. 發光的，放熱的；放射的，發射的。2. 【物理學】輻射性的。
  • forcing : n. 1. 強制，強奪。2. 【農業】催熟栽培。adj. 1. 強迫的，施加壓力的。2. 促成植物早熟的。
  1. The variations of sea ice in the arctic ocean are simulated by using a improved high resolution hibler dynamic - thermodynamic sea ice model during 1979 - 1998. the model is driven by surface atmospheric and oceanic forcing consists of geostrophic winds, surface air temperature, specific humidity, and longwave and shortwave radiative fluxes provided by international arctic buoy program ( iabp ). the simulated results show that arctic sea ice have noticeable seasonal and annual variability

    利用一個hibler海冰熱動力模式，在改進了其熱力部分和改變模擬范圍以及提高解析度的基礎上，以北極國際浮標計劃（ iabp ）提供的1979 - 1998年間逐日變化的日平均海平面氣溫場，濕度場，長短波輻射場，風場，洋流場，海洋熱流量場為強迫場，模擬了上述20年間北極海冰的時空演變。
  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. 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。
  4. Global warming potentials take into account the differing atmospheric lifetimes and abilities of various gases to absorb radiation. derivations of gwps requires knowledge of the fate of the emitted gas ( typically not well understood ) and the radiative forcing due to the amount remaining in the atmosphere ( reasonably well understood )

    在計算『全球變暖潛能』的時候，是需要明了各溫室氣體在大氣層中的演變情況（通常不太了解）和它們在大氣層的餘量所產生的輻射力（比較清楚知道） 。因此， 『全球變暖潛能』含有一些不確定因素，以co
  5. Analyzed the relationship between the cloud shortwave radiative forcing and the surface net radiative flux, the results were show by means of chart. the satellite grey values were get form the gms satellite data. analyzing the relationship between the cloud shortwave radiative forcing and the satellite grey values, established five regression equations and discussed them, select the best pattern, by which we can estimate the cloud shortwave radiative forcing

    同時利用gms衛星紅外和可見光兩個通道的數字雲圖資料，經過處理，分別得出雲圖的灰度計數值，分析了短波雲輻射強迫和衛星計數值的關系，並運用回歸方法建立了估算短波雲輻射強迫的五種模式，對五種模式進一步討論比較，得到估算短波雲輻射強迫的可用模式，用於短波雲輻射強迫的估算。
  6. A radiative forcing perturbs the balance between incoming and outgoing radiation

    輻射力影響了地球吸收和釋放輻射的平衡。
  7. It is thought that cfc - 11 and cfc - 12 have contributed about one - third of the radiative forcing of gases other than co

    以外， cfc - 11及cfc - 12在所有溫室氣體中對輻射力的影響已佔了三份之一。
  8. A positive radiative forcing tends on average to warm the earth s surface ; a negative radiative forcing tends on average to cool the earth s surface

    正值的輻射力會使地球表面變暖，負值的輻射力使地球表面變涼。
  9. Characteristics of surface radiative fluxes and cloud - radiative forcing with a focus on the arctic

    北極地區地面輻射量和雲輻射強迫特徵
  10. The cloud shortwave radiative forcing was studied by using gms satellite data and the routine data in the typical 9 stations in the paper

    本文利用gms衛星資料和常規資料研究雲對輻射的作用，對中國大陸地區比較有代表性的九個站點夏季每日08 、 09 、 10時的短波雲輻射強迫進行了研究。
  11. 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。
  12. It was demonstrated that in june and december, as far as the daily averaged rates were concerned, whether the aerosol concentration is the heat source or the cold one depends on the aerosol density. however, the relation bears nonlinear features. in the diurnal range, the effects of the aerosol radiative forcing on the atmospheric stability depend on the vertical distribution and density of the aerosol

    結果表明，從氣候角度而言，氣溶膠濃度的差別使得即使是在6月份，氣溶膠層既可以是冷源也可以是熱源從天氣尺度而言，氣溶膠的垂直分佈和濃度對層結穩定度有著重要影響，並由此從物理上指出了沙塵暴天氣過程中輻射效應所起的重要作用。
  13. Gwp reflects the relative strength of individual greenhouse gas with respect to its impact on global warming. it was defined as the cumulative radiative forcing between the present and some future time caused by a unit mass of greenhouse gas emitted now, expressed relative to co

    『全球變暖潛能』是反映溫室氣體的相對強度，其定義是指某一單位質量的溫室氣體在一定時間內相對于co
  14. It was defined as the cumulative radiative forcing between the present and some future time caused by a unit mass of greenhouse gas emitted now, expressed relative to co

    全球變暖潛能是反映溫室氣體的相對強度，其定義是指某一單位質量的溫室氣體在一定時間內相對于co
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