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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >LIFETIME AND EMISSION ESTIMATES OF 1,1,2-TRICHLOROTRIFLUORETHANE (CFC-113) FROM DAILY GLOBAL BACKGROUND OBSERVATIONS JUNE 1982 JUNE 1994
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LIFETIME AND EMISSION ESTIMATES OF 1,1,2-TRICHLOROTRIFLUORETHANE (CFC-113) FROM DAILY GLOBAL BACKGROUND OBSERVATIONS JUNE 1982 JUNE 1994

机译:从每日全球背景观测中估算1,1,2-三氟三氟乙烷(CFC-113)的寿命和排放1982年6月1994年6月

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摘要

Observations every two hours of CCl2FCClF2 at Mace Head, Ireland (February 1987-June 1994); Cape Meares, Oregon (April 1984-June 1989); Ragged Point, Barbados (October 1985-June 1994); Cape Matatula, Samoa (October 1985-June 1989 and January 1992-June 1994); and Cape Grim, Tasmania (June 1982-June 1994) are reported, The observations from Cape Grim have been extended back to 1978 using archived air samples. The global atmospheric abundance of CCl2FCClF2 is indicated to have been growing exponentially between 1978 and 1987 with an e-folding time of approximately 7.6 years; it has been growing less rapidly since that time. On January 1, 1994, the mean inferred northern hemispheric mixing ratio in the lower troposphere was 84.4 +/- 0.4 ppt and the southern hemispheric value was 80.6 +/- 0.4 ppt; the global growth rate in 1991-1993 is estimated to have averaged approximately 3.1 +/- 0.1 ppt/year. The differences between the northern and southern hemispheric concentrations are calculated to be consistent with the almost entirely northern hemispheric release of this gas. The annual release estimates of CCl2FCClF2 by industry, which include estimates of eastern European emissions, fairly consistently exceed those deduced from the measurements by approximately 10% from 1980 to 1993. The uncertainties in each estimate is approximately 5%. This difference suggests that up to 10% of past production might not yet have been released. The measurements indicate that atmospheric releases of CCl2FCClF2 have been decreasing rapidly since 1989 and in 1993 amounted to 78 +/- 27 x 10(6) kg or 42 +/- 15% of the 1985-1987 emissions. [References: 46]
机译:每两小时在爱尔兰梅斯黑德(Mace Head)观测一次CCl2FCClF2(1987年2月至1994年6月);俄勒冈州米勒斯角(1984年4月至1989年6月);巴巴多斯的衣衫Point的点(1985年10月至1994年6月);萨摩亚的Matatula角(1985年10月至1989年6月和1992年1月至1994年6月);以及塔斯马尼亚州格里姆角(1982年6月至1994年6月)的报道。格里姆角的观测已扩展至1978年,使用的是已存档的空气样本。 CCl2FCClF2的全球大气丰度被表明在1978年至1987年之间呈指数增长,其电子折叠时间约为7.6年。自那时以来,它的增长速度一直较慢。 1994年1月1日,对流层下层北半球的平均推断混合比为84.4 +/- 0.4 ppt,南半球为80.6 +/- 0.4 ppt。 1991-1993年的全球增长率估计平均每年约为3.1 +/- 0.1个百分点。计算得出的北半球和南半球浓度之间的差异与该气体几乎完全北半球的排放量一致。从1980年到1993年,按行业划分的CCl2FCClF2的年度排放估算值(包括东欧排放量的估算值)始终稳定地超过从这些估算值得出的估算值约10%。每个估算值的不确定性约为5%。这种差异表明,可能尚未释放过往产量的10%。测量结果表明,自1989年以来,CCl2FCClF2的大气排放量一直在迅速减少,1993年达到78 +/- 27 x 10(6)kg或1985-1987年排放量的42 +/- 15%。 [参考:46]

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