atmospheric forcing 中文意思是什麼

atmospheric forcing 解釋
大氣外力作用
  • atmospheric : adj. 1. 大氣（中）的。2. 大氣所致的。3. 空氣的。4. 氣壓的。5. 有…氣氛的。adj. -ical ,-ically adv. 在大氣影響下，氣壓上。
  • 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. 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
  3. Adjustment of the north atlantic thermohaline circulation to the atmospheric forcing in a global air - sea coupled model

    全球海氣耦合模式中熱鹽環流對大氣強迫的響應
  4. 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。
  5. 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。
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