Total ozone and perturbations in the middle stratosphere
Abstract Total ozone amounts are shown to vary with the motion systems of the stratospheric polar vortex. Two cold outbreaks, one over Europe in 1959 and the other over North America in 1960, produced similar pronounced minima in the total ozone records. The results support the hypothesis that major...
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crwiley:10.1002/qj.49708737404 2024-09-15T18:31:16+00:00 Total ozone and perturbations in the middle stratosphere Boville, B. W. Hare, F. K. 1961 http://dx.doi.org/10.1002/qj.49708737404 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49708737404 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49708737404 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Quarterly Journal of the Royal Meteorological Society volume 87, issue 374, page 490-501 ISSN 0035-9009 1477-870X journal-article 1961 crwiley https://doi.org/10.1002/qj.49708737404 2024-07-30T04:19:40Z Abstract Total ozone amounts are shown to vary with the motion systems of the stratospheric polar vortex. Two cold outbreaks, one over Europe in 1959 and the other over North America in 1960, produced similar pronounced minima in the total ozone records. The results support the hypothesis that major anomalies in the horizontal and seasonal distributions of total ozone are related to dynamical activity in the polar‐night vortex and the stratospheric warm belt. Article in Journal/Newspaper polar night Wiley Online Library Quarterly Journal of the Royal Meteorological Society 87 374 490 501 |
institution |
Open Polar |
collection |
Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Total ozone amounts are shown to vary with the motion systems of the stratospheric polar vortex. Two cold outbreaks, one over Europe in 1959 and the other over North America in 1960, produced similar pronounced minima in the total ozone records. The results support the hypothesis that major anomalies in the horizontal and seasonal distributions of total ozone are related to dynamical activity in the polar‐night vortex and the stratospheric warm belt. |
format |
Article in Journal/Newspaper |
author |
Boville, B. W. Hare, F. K. |
spellingShingle |
Boville, B. W. Hare, F. K. Total ozone and perturbations in the middle stratosphere |
author_facet |
Boville, B. W. Hare, F. K. |
author_sort |
Boville, B. W. |
title |
Total ozone and perturbations in the middle stratosphere |
title_short |
Total ozone and perturbations in the middle stratosphere |
title_full |
Total ozone and perturbations in the middle stratosphere |
title_fullStr |
Total ozone and perturbations in the middle stratosphere |
title_full_unstemmed |
Total ozone and perturbations in the middle stratosphere |
title_sort |
total ozone and perturbations in the middle stratosphere |
publisher |
Wiley |
publishDate |
1961 |
url |
http://dx.doi.org/10.1002/qj.49708737404 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49708737404 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49708737404 |
genre |
polar night |
genre_facet |
polar night |
op_source |
Quarterly Journal of the Royal Meteorological Society volume 87, issue 374, page 490-501 ISSN 0035-9009 1477-870X |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/qj.49708737404 |
container_title |
Quarterly Journal of the Royal Meteorological Society |
container_volume |
87 |
container_issue |
374 |
container_start_page |
490 |
op_container_end_page |
501 |
_version_ |
1810472898634186752 |