關於全球暖化文章(共3段)~英翻中~不要用翻譯軟體唷! - 暖化
By Joe
at 2009-05-18T00:00
at 2009-05-18T00:00
Table of Contents
一*Where IFSO2F2, IFCFC-11, MSO2F2, MCFC-11, τSO2F2, and τCFC-11 are the instantaneous forcings, molecular weights, and atmo-spheric of SO2F2 and CFC-11, and t is the time horizon over which the forcing is integrated.
二*We assume τCFC-11= 45 years. For the purposes of illustrating the potential order of magnitude contribution of SO2F2 to radiative forcing of climate we have considered a range of atmospheric lifetimes for SO2F2 of 1-100 years (centered on the value of 10 years discussed above and varied by an order of magnitude).
三*The GWP for SO2F2 relative to CO2 is estimated by multiplying the HGWP values for 20, 100, and 500 year time horizons by factors of 6730,4750, and 1620, respectively. Figure 3 shows the GWP of SO2F2 for 20, 100, and 500 year time horizons as a function of the atmospheric lifetime of SO2F2 leads to considerable uncertainty its GWP (120-7600 for a 100 year time horizon).
Update:
那請問這一段又該怎麼翻好呢?
The fact that we, Dillon et al.,and Papadimitriou et al.Have been not able to identify any significant atmospheric sink for SO2F2
Update 2:
接下來是underscores the need for improved docu-mentation of emission rates , atmospheric abundance trends, and potential oceanic or terrestrial sinks for this compound.
二*We assume τCFC-11= 45 years. For the purposes of illustrating the potential order of magnitude contribution of SO2F2 to radiative forcing of climate we have considered a range of atmospheric lifetimes for SO2F2 of 1-100 years (centered on the value of 10 years discussed above and varied by an order of magnitude).
三*The GWP for SO2F2 relative to CO2 is estimated by multiplying the HGWP values for 20, 100, and 500 year time horizons by factors of 6730,4750, and 1620, respectively. Figure 3 shows the GWP of SO2F2 for 20, 100, and 500 year time horizons as a function of the atmospheric lifetime of SO2F2 leads to considerable uncertainty its GWP (120-7600 for a 100 year time horizon).
Update:
那請問這一段又該怎麼翻好呢?
The fact that we, Dillon et al.,and Papadimitriou et al.Have been not able to identify any significant atmospheric sink for SO2F2
Update 2:
接下來是underscores the need for improved docu-mentation of emission rates , atmospheric abundance trends, and potential oceanic or terrestrial sinks for this compound.
Tags:
暖化
All Comments
By Rae
at 2009-05-20T09:28
at 2009-05-20T09:28
一、在此IFSO2F2、IFCFC-11、MSO2F2、MCFC-11、τSO2F2、與τCFC-11指的是SO2F2的瞬間力量、SO2F2的分子重量、SO2F2的大氣、CFC-11的大氣與SO2F2與CFC-11作用力整合的時間橫軸。
二*We assume τCFC-11= 45 years. For the purposes of illustrating the potential order of magnitude contribution of SO2F2 to radiative forcing of climate we have considered a range of atmospheric lifetimes for SO2F2 of 1-100 years (centered on the value of 10 years discussed above and varied by an order of magnitude).
二、我們假設τCFC-11等於45年。為了說明SO2F2的潛在順序對氣侯輻射力的巨大影響,我們考慮將SO2F2的大氣範圍設為1到100年 (以先前所討論的10年為中心,且以大小順序來改變)。
三*The GWP for SO2F2 relative to CO2 is estimated by multiplying the HGWP values for 20, 100, and 500 year time horizons by factors of 6730,4750, and 1620, respectively. Figure 3 shows the GWP of SO2F2 for 20, 100, and 500 year time horizons as a function of the atmospheric lifetime of SO2F2 leads to considerable uncertainty its GWP (120-7600 for a 100 year time horizon).
三、相對於CO2的SO2F2之GWP,乘以HGWP之值,對於時間橫軸20、50與100年,參數分別取6730,4750與1620。圖三顯示SO2F2之GWP對於時間橫軸20、50與100年的圖,可看做是SO2F2的大氣生命週期的函數,從此圖推導出一相當不穩定的GWP (對於時間橫軸100年而言,約120-7600)。
2009-05-21 09:46:06 補充:
我將有些英文拼字重排了一下:
The fact that we, Dillon et al., and Papadimitriou et al. have been not able to identify any significant atmospheric sink for SO2F2 underscores the need for improved
2009-05-21 09:46:15 補充:
documentation of emission rates, atmospheric abundance trends, and potential oceanic or terrestrial sinks for this compound.
2009-05-21 09:48:39 補充:
我們等人,包括Dillon與Papadimitriou等,皆已無法分辨任何SO2F2的明顯大氣衰減,此一事實強調了一些改善文件的需求 (不直譯:從此一事實中,我們知道我們仍需要一些改善文件),這些文件包含散發率、大氣飽足趨勢,與潛在的整體海洋或大陸的衰減。
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