Four decades of ozonesonde measurements over antarctica
described and intercompared. Observations from the two sites reveal remarkable agreement, supporting and extending the understanding gained from either individually. Both sites exhibit extensive Antarctic ozone losses in a relatively narrow altitude range from about 12 to 24 km in October, and the d...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.409.1368 2023-05-15T14:00:01+02:00 Four decades of ozonesonde measurements over antarctica Susan Solomon Robert W. Portmann Toru Sasaki David J. Hofmann David W. J. Thompson The Pennsylvania State University CiteSeerX Archives 2005 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.409.1368 http://www.image.ucar.edu/idag/Papers/Solomon_ozonesonde.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.409.1368 http://www.image.ucar.edu/idag/Papers/Solomon_ozonesonde.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.image.ucar.edu/idag/Papers/Solomon_ozonesonde.pdf text 2005 ftciteseerx 2016-01-08T03:11:53Z described and intercompared. Observations from the two sites reveal remarkable agreement, supporting and extending the understanding gained from either individually. Both sites exhibit extensive Antarctic ozone losses in a relatively narrow altitude range from about 12 to 24 km in October, and the data are consistent with temperaturedependent chemistry involving chlorine on polar stratospheric clouds as the cause of the ozone hole. The maximum October ozone losses at higher altitudes near 18 km (70 hPa) appear to be transported to lower levels near the tropopause on a timescale of a few months, which is likely to affect the timing of the effects of ozone depletion on possible tropospheric climate changes. Both sites also show greater ozone losses in the lowermost stratosphere after the volcanic eruption of Mt. Pinatubo, supporting the view that surface chemistry can be enhanced by volcanic perturbations and that the very deep ozone holes observed in the early 1990s reflected such enhancements. Sparse data from the Syowa station in the early 1980s also suggest that enhanced ozone losses due to the El Chichon eruption may have contributed to the beginning of a measurable ozone hole. Observations at both locations show that some ozone depletion now occurs during much if not all year at lower altitudes near 12–14 km. Correlations between temperature and ozone provide new insights into ozone losses, including its nonlinear character, maximum effectiveness, and utility as a tool to distinguish dynamical effects from chemical processes. These data also show that recent changes in ozone do not yet indicate ozone recovery linked to changing chlorine abundances but provide new tools to probe observations for the first such future signals. Text Antarc* Antarctic Antarctica Unknown Antarctic Syowa Station |
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English |
description |
described and intercompared. Observations from the two sites reveal remarkable agreement, supporting and extending the understanding gained from either individually. Both sites exhibit extensive Antarctic ozone losses in a relatively narrow altitude range from about 12 to 24 km in October, and the data are consistent with temperaturedependent chemistry involving chlorine on polar stratospheric clouds as the cause of the ozone hole. The maximum October ozone losses at higher altitudes near 18 km (70 hPa) appear to be transported to lower levels near the tropopause on a timescale of a few months, which is likely to affect the timing of the effects of ozone depletion on possible tropospheric climate changes. Both sites also show greater ozone losses in the lowermost stratosphere after the volcanic eruption of Mt. Pinatubo, supporting the view that surface chemistry can be enhanced by volcanic perturbations and that the very deep ozone holes observed in the early 1990s reflected such enhancements. Sparse data from the Syowa station in the early 1980s also suggest that enhanced ozone losses due to the El Chichon eruption may have contributed to the beginning of a measurable ozone hole. Observations at both locations show that some ozone depletion now occurs during much if not all year at lower altitudes near 12–14 km. Correlations between temperature and ozone provide new insights into ozone losses, including its nonlinear character, maximum effectiveness, and utility as a tool to distinguish dynamical effects from chemical processes. These data also show that recent changes in ozone do not yet indicate ozone recovery linked to changing chlorine abundances but provide new tools to probe observations for the first such future signals. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Susan Solomon Robert W. Portmann Toru Sasaki David J. Hofmann David W. J. Thompson |
spellingShingle |
Susan Solomon Robert W. Portmann Toru Sasaki David J. Hofmann David W. J. Thompson Four decades of ozonesonde measurements over antarctica |
author_facet |
Susan Solomon Robert W. Portmann Toru Sasaki David J. Hofmann David W. J. Thompson |
author_sort |
Susan Solomon |
title |
Four decades of ozonesonde measurements over antarctica |
title_short |
Four decades of ozonesonde measurements over antarctica |
title_full |
Four decades of ozonesonde measurements over antarctica |
title_fullStr |
Four decades of ozonesonde measurements over antarctica |
title_full_unstemmed |
Four decades of ozonesonde measurements over antarctica |
title_sort |
four decades of ozonesonde measurements over antarctica |
publishDate |
2005 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.409.1368 http://www.image.ucar.edu/idag/Papers/Solomon_ozonesonde.pdf |
geographic |
Antarctic Syowa Station |
geographic_facet |
Antarctic Syowa Station |
genre |
Antarc* Antarctic Antarctica |
genre_facet |
Antarc* Antarctic Antarctica |
op_source |
http://www.image.ucar.edu/idag/Papers/Solomon_ozonesonde.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.409.1368 http://www.image.ucar.edu/idag/Papers/Solomon_ozonesonde.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766268994126348288 |