Ozone trend and the stratospheric circulation over Australia
Abstract Trends in total ozone for the period 1963–1974 at Australian stations Darwin, Brisbane, Aspendale and Macquarie Island have been discussed. Only Aspendale has a decreasing trend, which may be statistically significant. Trends in ozone at other places are not statistically significant. From...
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crwiley:10.1002/qj.49710243314 2024-06-02T08:10:15+00:00 Ozone trend and the stratospheric circulation over Australia Kulkarni, R. N. 1976 http://dx.doi.org/10.1002/qj.49710243314 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49710243314 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49710243314 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Quarterly Journal of the Royal Meteorological Society volume 102, issue 433, page 697-703 ISSN 0035-9009 1477-870X journal-article 1976 crwiley https://doi.org/10.1002/qj.49710243314 2024-05-03T11:46:58Z Abstract Trends in total ozone for the period 1963–1974 at Australian stations Darwin, Brisbane, Aspendale and Macquarie Island have been discussed. Only Aspendale has a decreasing trend, which may be statistically significant. Trends in ozone at other places are not statistically significant. From the trend analysis of temperature at the 100mb level, and from Umkehr analysis, it is concluded that the changes in circulation in the lower stratosphere are sufficient to explain the observed trends. Article in Journal/Newspaper Macquarie Island Wiley Online Library Brisbane ENVELOPE(-45.633,-45.633,-60.600,-60.600) Quarterly Journal of the Royal Meteorological Society 102 433 697 703 |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Trends in total ozone for the period 1963–1974 at Australian stations Darwin, Brisbane, Aspendale and Macquarie Island have been discussed. Only Aspendale has a decreasing trend, which may be statistically significant. Trends in ozone at other places are not statistically significant. From the trend analysis of temperature at the 100mb level, and from Umkehr analysis, it is concluded that the changes in circulation in the lower stratosphere are sufficient to explain the observed trends. |
format |
Article in Journal/Newspaper |
author |
Kulkarni, R. N. |
spellingShingle |
Kulkarni, R. N. Ozone trend and the stratospheric circulation over Australia |
author_facet |
Kulkarni, R. N. |
author_sort |
Kulkarni, R. N. |
title |
Ozone trend and the stratospheric circulation over Australia |
title_short |
Ozone trend and the stratospheric circulation over Australia |
title_full |
Ozone trend and the stratospheric circulation over Australia |
title_fullStr |
Ozone trend and the stratospheric circulation over Australia |
title_full_unstemmed |
Ozone trend and the stratospheric circulation over Australia |
title_sort |
ozone trend and the stratospheric circulation over australia |
publisher |
Wiley |
publishDate |
1976 |
url |
http://dx.doi.org/10.1002/qj.49710243314 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49710243314 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49710243314 |
long_lat |
ENVELOPE(-45.633,-45.633,-60.600,-60.600) |
geographic |
Brisbane |
geographic_facet |
Brisbane |
genre |
Macquarie Island |
genre_facet |
Macquarie Island |
op_source |
Quarterly Journal of the Royal Meteorological Society volume 102, issue 433, page 697-703 ISSN 0035-9009 1477-870X |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/qj.49710243314 |
container_title |
Quarterly Journal of the Royal Meteorological Society |
container_volume |
102 |
container_issue |
433 |
container_start_page |
697 |
op_container_end_page |
703 |
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1800756089977831424 |