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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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) |
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NASA Technical Reports Server (NTRS) |
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ftnasantrs |
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46 |
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46 Rood, Richard B. Global ozone minima in the historical record |
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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 |
_version_ |
1766270732426280960 |