Antarctic Ozone Depletion and Trends in Tropopause Rossby Wave Breaking ...

Trends in summer tropopause Rossby wave breaking (RWB) are examined using meteorological reanalyses and model integrations. The reanalyses for the last 30 years show large increases in RWB on the equatorward side of the tropospheric jet and weak decreases on the poleward side. Comparable changes in...

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Bibliographic Details
Main Authors: Ndarana, T., Waugh, D. W., Polvani, Lorenzo M., Correa, Gustavo P., Gerber, E. P.
Format: Article in Journal/Newspaper
Language:unknown
Published: Columbia University 2012
Subjects:
Online Access:https://dx.doi.org/10.7916/d8kd1xcx
https://academiccommons.columbia.edu/doi/10.7916/D8KD1XCX
id ftdatacite:10.7916/d8kd1xcx
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spelling ftdatacite:10.7916/d8kd1xcx 2024-10-13T14:03:21+00:00 Antarctic Ozone Depletion and Trends in Tropopause Rossby Wave Breaking ... Ndarana, T. Waugh, D. W. Polvani, Lorenzo M. Correa, Gustavo P. Gerber, E. P. 2012 https://dx.doi.org/10.7916/d8kd1xcx https://academiccommons.columbia.edu/doi/10.7916/D8KD1XCX unknown Columbia University https://dx.doi.org/10.1002/asl.384 Atmosphere Meteorology Climatic changes Text article-journal Articles ScholarlyArticle 2012 ftdatacite https://doi.org/10.7916/d8kd1xcx10.1002/asl.384 2024-10-01T11:37:24Z Trends in summer tropopause Rossby wave breaking (RWB) are examined using meteorological reanalyses and model integrations. The reanalyses for the last 30 years show large increases in RWB on the equatorward side of the tropospheric jet and weak decreases on the poleward side. Comparable changes in RWB are found in general circulation model integrations whose stratospheric ozone differs between 1960 and 2000 levels, but not in integrations that differ only in their greenhouse gas concentrations and sea-surface temperatures. These results indicate that the formation of the ozone hole has led to changes in RWB frequency during southern summer. ... Article in Journal/Newspaper Antarc* Antarctic DataCite Antarctic
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language unknown
topic Atmosphere
Meteorology
Climatic changes
spellingShingle Atmosphere
Meteorology
Climatic changes
Ndarana, T.
Waugh, D. W.
Polvani, Lorenzo M.
Correa, Gustavo P.
Gerber, E. P.
Antarctic Ozone Depletion and Trends in Tropopause Rossby Wave Breaking ...
topic_facet Atmosphere
Meteorology
Climatic changes
description Trends in summer tropopause Rossby wave breaking (RWB) are examined using meteorological reanalyses and model integrations. The reanalyses for the last 30 years show large increases in RWB on the equatorward side of the tropospheric jet and weak decreases on the poleward side. Comparable changes in RWB are found in general circulation model integrations whose stratospheric ozone differs between 1960 and 2000 levels, but not in integrations that differ only in their greenhouse gas concentrations and sea-surface temperatures. These results indicate that the formation of the ozone hole has led to changes in RWB frequency during southern summer. ...
format Article in Journal/Newspaper
author Ndarana, T.
Waugh, D. W.
Polvani, Lorenzo M.
Correa, Gustavo P.
Gerber, E. P.
author_facet Ndarana, T.
Waugh, D. W.
Polvani, Lorenzo M.
Correa, Gustavo P.
Gerber, E. P.
author_sort Ndarana, T.
title Antarctic Ozone Depletion and Trends in Tropopause Rossby Wave Breaking ...
title_short Antarctic Ozone Depletion and Trends in Tropopause Rossby Wave Breaking ...
title_full Antarctic Ozone Depletion and Trends in Tropopause Rossby Wave Breaking ...
title_fullStr Antarctic Ozone Depletion and Trends in Tropopause Rossby Wave Breaking ...
title_full_unstemmed Antarctic Ozone Depletion and Trends in Tropopause Rossby Wave Breaking ...
title_sort antarctic ozone depletion and trends in tropopause rossby wave breaking ...
publisher Columbia University
publishDate 2012
url https://dx.doi.org/10.7916/d8kd1xcx
https://academiccommons.columbia.edu/doi/10.7916/D8KD1XCX
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation https://dx.doi.org/10.1002/asl.384
op_doi https://doi.org/10.7916/d8kd1xcx10.1002/asl.384
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