Satellite maps of Antarctic total ozone
Satellite remote sensing techniques for ozone have made it possible to observe the detailed, daily horizontal structure of atmospheric ozone at all locations where sunlight is present. The Antarctic ozone 'hole' has been observed with the Total Ozone Mapping Spectrometer (TOMS) instrument...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19880034927 2023-05-15T13:41:01+02:00 Satellite maps of Antarctic total ozone Krueger, Arlin J. Unclassified, Unlimited, Publicly available Jan 1, 1988 http://ntrs.nasa.gov/search.jsp?R=19880034927 unknown http://ntrs.nasa.gov/search.jsp?R=19880034927 Accession ID: 88A22154 Copyright Other Sources 46 AIAA PAPER 88-0210 1988 ftnasantrs 2012-02-15T17:32:08Z Satellite remote sensing techniques for ozone have made it possible to observe the detailed, daily horizontal structure of atmospheric ozone at all locations where sunlight is present. The Antarctic ozone 'hole' has been observed with the Total Ozone Mapping Spectrometer (TOMS) instrument since launch of Nimbus 7 in 1978. This feature is a continental-size ozone minimum found in the Antarctic winter and spring seasons which has generally deepened in recent years to levels in 1985 and 1987 far below the lowest values ever observed elsewhere. The minimum appears to be produced by atmospheric circulations, but the deepening almost certainly involves chemistry which is unique to cold, dark conditions. 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 Krueger, Arlin J. Satellite maps of Antarctic total ozone |
topic_facet |
46 |
description |
Satellite remote sensing techniques for ozone have made it possible to observe the detailed, daily horizontal structure of atmospheric ozone at all locations where sunlight is present. The Antarctic ozone 'hole' has been observed with the Total Ozone Mapping Spectrometer (TOMS) instrument since launch of Nimbus 7 in 1978. This feature is a continental-size ozone minimum found in the Antarctic winter and spring seasons which has generally deepened in recent years to levels in 1985 and 1987 far below the lowest values ever observed elsewhere. The minimum appears to be produced by atmospheric circulations, but the deepening almost certainly involves chemistry which is unique to cold, dark conditions. |
format |
Other/Unknown Material |
author |
Krueger, Arlin J. |
author_facet |
Krueger, Arlin J. |
author_sort |
Krueger, Arlin J. |
title |
Satellite maps of Antarctic total ozone |
title_short |
Satellite maps of Antarctic total ozone |
title_full |
Satellite maps of Antarctic total ozone |
title_fullStr |
Satellite maps of Antarctic total ozone |
title_full_unstemmed |
Satellite maps of Antarctic total ozone |
title_sort |
satellite maps of antarctic total ozone |
publishDate |
1988 |
url |
http://ntrs.nasa.gov/search.jsp?R=19880034927 |
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=19880034927 Accession ID: 88A22154 |
op_rights |
Copyright |
_version_ |
1766144363653496832 |