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对臭氧层恢复迹象的探寻。

The search for signs of recovery of the ozone layer.

作者信息

Weatherhead Elizabeth C, Andersen Signe Bech

机构信息

Cooperative Institute for Research in Environmental Science, Campus Box 216, University of Colorado, Boulder, Colorado 80307, USA.

出版信息

Nature. 2006 May 4;441(7089):39-45. doi: 10.1038/nature04746.

Abstract

Evidence of mid-latitude ozone depletion and proof that the Antarctic ozone hole was caused by humans spurred policy makers from the late 1980s onwards to ratify the Montreal Protocol and subsequent treaties, legislating for reduced production of ozone-depleting substances. The case of anthropogenic ozone loss has often been cited since as a success story of international agreements in the regulation of environmental pollution. Although recent data suggest that total column ozone abundances have at least not decreased over the past eight years for most of the world, it is still uncertain whether this improvement is actually attributable to the observed decline in the amount of ozone-depleting substances in the Earth's atmosphere. The high natural variability in ozone abundances, due in part to the solar cycle as well as changes in transport and temperature, could override the relatively small changes expected from the recent decrease in ozone-depleting substances. Whatever the benefits of the Montreal agreement, recovery of ozone is likely to occur in a different atmospheric environment, with changes expected in atmospheric transport, temperature and important trace gases. It is therefore unlikely that ozone will stabilize at levels observed before 1980, when a decline in ozone concentrations was first observed.

摘要

中纬度地区臭氧损耗的证据以及南极臭氧空洞是由人类活动造成的这一证明,促使政策制定者从20世纪80年代末开始批准《蒙特利尔议定书》及后续条约,立法减少消耗臭氧层物质的生产。自那以后,人为造成臭氧损耗的案例经常被引述为国际协定在环境污染监管方面的成功范例。尽管最近的数据表明,在过去八年里,世界上大部分地区的总臭氧柱丰度至少没有下降,但这种改善是否真的归因于地球大气中消耗臭氧层物质数量的减少仍不确定。臭氧丰度存在很大的自然变率,部分原因是太阳活动周期以及传输和温度的变化,这可能会掩盖因近期消耗臭氧层物质减少而预期出现的相对较小的变化。无论《蒙特利尔协定》有何益处,臭氧的恢复可能会在一个不同的大气环境中发生,预计大气传输、温度和重要微量气体都会发生变化。因此,臭氧浓度不太可能稳定在1980年首次观测到下降之前的水平。

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