The Antarctic ozone minimum - Relationship to odd nitrogen, odd chlorine, the final warming, and the 11-year solar cycle
Photochemical calculations along 'diabatic trajectories' in the meridional phase are used to search for the cause of the dramatic springtime minimum in Antarctic column ozone. The results indicate that the minimum is principally due to catalytic destruction of ozone by high levels of total...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19870031802 2023-05-15T14:01:08+02:00 The Antarctic ozone minimum - Relationship to odd nitrogen, odd chlorine, the final warming, and the 11-year solar cycle Callis, L. B. Natarajan, M. Unclassified, Unlimited, Publicly available Sep 20, 1986 http://ntrs.nasa.gov/search.jsp?R=19870031802 unknown http://ntrs.nasa.gov/search.jsp?R=19870031802 Accession ID: 87A19076 Copyright Other Sources 46 Journal of Geophysical Research; 91; 10771-10 1986 ftnasantrs 2012-02-15T17:08:03Z Photochemical calculations along 'diabatic trajectories' in the meridional phase are used to search for the cause of the dramatic springtime minimum in Antarctic column ozone. The results indicate that the minimum is principally due to catalytic destruction of ozone by high levels of total odd nitrogen. Calculations suggest that these levels of odd nitrogen are transported within the polar vortex and during the polar night from the middle to upper stratosphere and lower mesosphere to the lower stratosphere. The possibility that these levels are related to the 11-year solar cycle and are increased by enhanced formation in the thermosphere and mesosphere during solar maximum conditions is discussed. Other/Unknown Material Antarc* Antarctic polar night NASA Technical Reports Server (NTRS) Antarctic The Antarctic |
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NASA Technical Reports Server (NTRS) |
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ftnasantrs |
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46 |
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46 Callis, L. B. Natarajan, M. The Antarctic ozone minimum - Relationship to odd nitrogen, odd chlorine, the final warming, and the 11-year solar cycle |
topic_facet |
46 |
description |
Photochemical calculations along 'diabatic trajectories' in the meridional phase are used to search for the cause of the dramatic springtime minimum in Antarctic column ozone. The results indicate that the minimum is principally due to catalytic destruction of ozone by high levels of total odd nitrogen. Calculations suggest that these levels of odd nitrogen are transported within the polar vortex and during the polar night from the middle to upper stratosphere and lower mesosphere to the lower stratosphere. The possibility that these levels are related to the 11-year solar cycle and are increased by enhanced formation in the thermosphere and mesosphere during solar maximum conditions is discussed. |
format |
Other/Unknown Material |
author |
Callis, L. B. Natarajan, M. |
author_facet |
Callis, L. B. Natarajan, M. |
author_sort |
Callis, L. B. |
title |
The Antarctic ozone minimum - Relationship to odd nitrogen, odd chlorine, the final warming, and the 11-year solar cycle |
title_short |
The Antarctic ozone minimum - Relationship to odd nitrogen, odd chlorine, the final warming, and the 11-year solar cycle |
title_full |
The Antarctic ozone minimum - Relationship to odd nitrogen, odd chlorine, the final warming, and the 11-year solar cycle |
title_fullStr |
The Antarctic ozone minimum - Relationship to odd nitrogen, odd chlorine, the final warming, and the 11-year solar cycle |
title_full_unstemmed |
The Antarctic ozone minimum - Relationship to odd nitrogen, odd chlorine, the final warming, and the 11-year solar cycle |
title_sort |
antarctic ozone minimum - relationship to odd nitrogen, odd chlorine, the final warming, and the 11-year solar cycle |
publishDate |
1986 |
url |
http://ntrs.nasa.gov/search.jsp?R=19870031802 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic polar night |
genre_facet |
Antarc* Antarctic polar night |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19870031802 Accession ID: 87A19076 |
op_rights |
Copyright |
_version_ |
1766270730665721856 |