Climate Change and Atmospheric Chemistry: How Will the Stratospheric Ozone Layer Develop?
Abstract The discovery of the ozone hole over Antarctica in 1985 was a surprise for science. For a few years the reasons of the ozone hole was speculated about. Soon it was obvious that predominant meteorological conditions led to a specific situation developing in this part of the atmosphere: Very...
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crwiley:10.1002/anie.201001643 2024-09-15T17:42:29+00:00 Climate Change and Atmospheric Chemistry: How Will the Stratospheric Ozone Layer Develop? Dameris, Martin 2010 http://dx.doi.org/10.1002/anie.201001643 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fanie.201001643 https://onlinelibrary.wiley.com/doi/pdf/10.1002/anie.201001643 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Angewandte Chemie International Edition volume 49, issue 44, page 8092-8102 ISSN 1433-7851 1521-3773 journal-article 2010 crwiley https://doi.org/10.1002/anie.201001643 2024-08-27T04:31:17Z Abstract The discovery of the ozone hole over Antarctica in 1985 was a surprise for science. For a few years the reasons of the ozone hole was speculated about. Soon it was obvious that predominant meteorological conditions led to a specific situation developing in this part of the atmosphere: Very low temperatures initiate chemical processes that at the end cause extreme ozone depletion at altitudes of between about 15 and 30 km. So‐called polar stratospheric clouds play a key role. Such clouds develop at temperatures below about 195 K. Heterogeneous chemical reactions on cloud particles initiate the destruction of ozone molecules. The future evolution of the ozone layer will not only depend on the further development of concentrations of ozone‐depleting substances, but also significantly on climate change. Article in Journal/Newspaper Antarc* Antarctica Wiley Online Library Angewandte Chemie International Edition 49 44 8092 8102 |
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Abstract The discovery of the ozone hole over Antarctica in 1985 was a surprise for science. For a few years the reasons of the ozone hole was speculated about. Soon it was obvious that predominant meteorological conditions led to a specific situation developing in this part of the atmosphere: Very low temperatures initiate chemical processes that at the end cause extreme ozone depletion at altitudes of between about 15 and 30 km. So‐called polar stratospheric clouds play a key role. Such clouds develop at temperatures below about 195 K. Heterogeneous chemical reactions on cloud particles initiate the destruction of ozone molecules. The future evolution of the ozone layer will not only depend on the further development of concentrations of ozone‐depleting substances, but also significantly on climate change. |
format |
Article in Journal/Newspaper |
author |
Dameris, Martin |
spellingShingle |
Dameris, Martin Climate Change and Atmospheric Chemistry: How Will the Stratospheric Ozone Layer Develop? |
author_facet |
Dameris, Martin |
author_sort |
Dameris, Martin |
title |
Climate Change and Atmospheric Chemistry: How Will the Stratospheric Ozone Layer Develop? |
title_short |
Climate Change and Atmospheric Chemistry: How Will the Stratospheric Ozone Layer Develop? |
title_full |
Climate Change and Atmospheric Chemistry: How Will the Stratospheric Ozone Layer Develop? |
title_fullStr |
Climate Change and Atmospheric Chemistry: How Will the Stratospheric Ozone Layer Develop? |
title_full_unstemmed |
Climate Change and Atmospheric Chemistry: How Will the Stratospheric Ozone Layer Develop? |
title_sort |
climate change and atmospheric chemistry: how will the stratospheric ozone layer develop? |
publisher |
Wiley |
publishDate |
2010 |
url |
http://dx.doi.org/10.1002/anie.201001643 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fanie.201001643 https://onlinelibrary.wiley.com/doi/pdf/10.1002/anie.201001643 |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Angewandte Chemie International Edition volume 49, issue 44, page 8092-8102 ISSN 1433-7851 1521-3773 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/anie.201001643 |
container_title |
Angewandte Chemie International Edition |
container_volume |
49 |
container_issue |
44 |
container_start_page |
8092 |
op_container_end_page |
8102 |
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1810489072148283392 |