Chemistry of the Antarctic stratosphere
Interferometric measurements of HCl, ClNO3, HNO3, NO2, and NO obtained over the Antarctic in 1986 are used to model the chemistry of the atmosphere in the region of the Ozone Hole. The low abundance noted in stratospheric HCl is attributed to incorporation of HCl in polar stratospheric clouds and su...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19880042145 2023-05-15T13:41:01+02:00 Chemistry of the Antarctic stratosphere Mcelroy, Michael B. Salawitch, Ross J. Wofsy, Steven C. Unclassified, Unlimited, Publicly available Jan 1, 1988 http://ntrs.nasa.gov/search.jsp?R=19880042145 unknown http://ntrs.nasa.gov/search.jsp?R=19880042145 Accession ID: 88A29372 Copyright Other Sources 46 Planetary and Space Science; 36; 73-87 1988 ftnasantrs 2012-02-15T17:34:35Z Interferometric measurements of HCl, ClNO3, HNO3, NO2, and NO obtained over the Antarctic in 1986 are used to model the chemistry of the atmosphere in the region of the Ozone Hole. The low abundance noted in stratospheric HCl is attributed to incorporation of HCl in polar stratospheric clouds and subsequent reaction of HCl with ClNO3. The results point to a net loss of HNO3 from the stratosphere and to the suppression of the abundance of odd nitrogen at high altitudes in the vortex. O3 loss is suggested to be due to the catalytic influence of halogen radicals. Other/Unknown Material Antarc* Antarctic NASA Technical Reports Server (NTRS) Antarctic The Antarctic |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
46 |
spellingShingle |
46 Mcelroy, Michael B. Salawitch, Ross J. Wofsy, Steven C. Chemistry of the Antarctic stratosphere |
topic_facet |
46 |
description |
Interferometric measurements of HCl, ClNO3, HNO3, NO2, and NO obtained over the Antarctic in 1986 are used to model the chemistry of the atmosphere in the region of the Ozone Hole. The low abundance noted in stratospheric HCl is attributed to incorporation of HCl in polar stratospheric clouds and subsequent reaction of HCl with ClNO3. The results point to a net loss of HNO3 from the stratosphere and to the suppression of the abundance of odd nitrogen at high altitudes in the vortex. O3 loss is suggested to be due to the catalytic influence of halogen radicals. |
format |
Other/Unknown Material |
author |
Mcelroy, Michael B. Salawitch, Ross J. Wofsy, Steven C. |
author_facet |
Mcelroy, Michael B. Salawitch, Ross J. Wofsy, Steven C. |
author_sort |
Mcelroy, Michael B. |
title |
Chemistry of the Antarctic stratosphere |
title_short |
Chemistry of the Antarctic stratosphere |
title_full |
Chemistry of the Antarctic stratosphere |
title_fullStr |
Chemistry of the Antarctic stratosphere |
title_full_unstemmed |
Chemistry of the Antarctic stratosphere |
title_sort |
chemistry of the antarctic stratosphere |
publishDate |
1988 |
url |
http://ntrs.nasa.gov/search.jsp?R=19880042145 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19880042145 Accession ID: 88A29372 |
op_rights |
Copyright |
_version_ |
1766144388416667648 |