Global ozone minima in the historical record

The magnitude and structure of the global total ozone minimum between 1958 and 1962 is similar to that observed between 1979 and 1983. Analysis of the single station data that exhibit the most pronounced minima suggest that the spatial structure of the global minimum is different from the currently...

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Main Author: Rood, Richard B.
Language:unknown
Published: 1986
Subjects:
46
Online Access:http://ntrs.nasa.gov/search.jsp?R=19870036264
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record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19870036264 2023-05-15T14:01:08+02:00 Global ozone minima in the historical record Rood, Richard B. Unclassified, Unlimited, Publicly available Nov 1, 1986 http://ntrs.nasa.gov/search.jsp?R=19870036264 unknown http://ntrs.nasa.gov/search.jsp?R=19870036264 Accession ID: 87A23538 Copyright Other Sources 46 1986 ftnasantrs 2012-02-15T17:09:53Z The magnitude and structure of the global total ozone minimum between 1958 and 1962 is similar to that observed between 1979 and 1983. Analysis of the single station data that exhibit the most pronounced minima suggest that the spatial structure of the global minimum is different from the currently observed reduction. Very low north polar values were observed, but there is no indication of anomalously low ozone in Antarctica. The temporal relationship to the sun spot cycle is similar in both time periods. Rather than solar terrestrial interaction, however, a more likely explanation of the early 1960's reduction is normal climatology caused by a persistent period of planetary wave activity. Such a natural explanation may also be appropriate for the current depletion. Other/Unknown Material Antarc* Antarctica NASA Technical Reports Server (NTRS)
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic 46
spellingShingle 46
Rood, Richard B.
Global ozone minima in the historical record
topic_facet 46
description The magnitude and structure of the global total ozone minimum between 1958 and 1962 is similar to that observed between 1979 and 1983. Analysis of the single station data that exhibit the most pronounced minima suggest that the spatial structure of the global minimum is different from the currently observed reduction. Very low north polar values were observed, but there is no indication of anomalously low ozone in Antarctica. The temporal relationship to the sun spot cycle is similar in both time periods. Rather than solar terrestrial interaction, however, a more likely explanation of the early 1960's reduction is normal climatology caused by a persistent period of planetary wave activity. Such a natural explanation may also be appropriate for the current depletion.
author Rood, Richard B.
author_facet Rood, Richard B.
author_sort Rood, Richard B.
title Global ozone minima in the historical record
title_short Global ozone minima in the historical record
title_full Global ozone minima in the historical record
title_fullStr Global ozone minima in the historical record
title_full_unstemmed Global ozone minima in the historical record
title_sort global ozone minima in the historical record
publishDate 1986
url http://ntrs.nasa.gov/search.jsp?R=19870036264
op_coverage Unclassified, Unlimited, Publicly available
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Other Sources
op_relation http://ntrs.nasa.gov/search.jsp?R=19870036264
Accession ID: 87A23538
op_rights Copyright
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