Environmental effects of ozone depletion and its interactions with climate change: Progress report, 2007

被引:0
作者
机构
来源
Photochemical & Photobiological Sciences | 2008年 / 7卷
关键词
D O I
暂无
中图分类号
学科分类号
摘要
This year the Montreal Protocol celebrates its 20th Anniversary. In September 1987, 24 countries signed the ‘Montreal Protocol on Substances that Deplete the Ozone Layer’. Today 191 countries have signed and have met strict commitments on phasing out of ozone depleting substances with the result that a 95% reduction of these substances has been achieved. The Montreal Protocol has also contributed to slowing the rate of global climate change, since most of the ozone depleting substances are also effective greenhouse gases. Even though much has been achieved, the future of the stratospheric ozone layer relies on full compliance of the Montreal Protocol by all countries for the remaining substances, includingmethyl bromide, as well as strict monitoring of potential risks from the production of substitute chemicals. Also the ozone depleting substances existing in banks and equipment need special attention to prevent their release to the stratosphere. Since many of the ozone depleting substances already in the atmosphere are long-lived, recovery cannot be immediate and present projections estimate a return to pre-1980 levels by 2050 to 2075. It has also been predicted that the interactions of the effects of the ozone layer and that of other climate change factors will become increasingly important.
引用
收藏
页码:15 / 27
页数:12
相关论文
共 800 条
[1]  
Stolarski R S(2006)Search for evidence of trend slow-down in the long-term TOMS/SBUV total ozone data record: the importance of instrument drift uncertainty Atmos. Chem. Phys. 6 4057-4065
[2]  
Frith S M(2007)The importance of the Montreal Protocol in protecting climate Proc. Natl. Acad. Sci. USA 104 4814-4819
[3]  
Velders G J M(2004)Southern Hemisphere climate response to ozone changes and greenhouse gas increases Geophys. Res. Lett. 31 L18209-1577
[4]  
Andersen S O(2007)How will the stratosphere affect climate change Science 316 1576-2101
[5]  
Daniel J S(2007)Nine years of UV aerosol optical depth measurements at Thessaloniki, Greece Atmos. Chem. Phys. 7 2091-371
[6]  
Fahey D W(2007)Attempts to probe the ozone layer and the UV-B levels of the past Ambio 36 366-8
[7]  
McFarland M(2007)Melanoma in children and teenagers: an analysis of patients from the National Cancer Data Base J. Clin. Oncol. 25 1363-1300
[8]  
Shindell D T(2007)Recent trends in incidence of nonmelanoma skin cancers in the East of Scotland, 1992-2003 Br. J. Dermatol. 156 1295-10
[9]  
Schmidt G A(2006)Non-melanoma skin cancer in Australia: the 2002 national survey and trends since 1985 Med. J. Aust. 184 6-7
[10]  
Baldwin M P(2007)Epidemiology of nonmelanoma skin cancer (NMSC) in Europe: accurate and comparable data are needed for effective public health monitoring and interventions Br. J. Opthalmol. 156 1-6