Observational evidence for the mechanism of the poleward propagation of zonal wind anomalies over the North Atlantic

Abstract This study examines the physical mechanisms that drive the poleward propagation of zonal‐mean flow anomalies over the North Atlantic during the boreal winter with ECMWF ERA40 reanalysis data that spans the years 1958–2001. An empirical orthogonal function (EOF) analysis is performed on the...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Yuan, Jiacan, Lee, Sukyoung, Tan, Benkui
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2012
Subjects:
Online Access:http://dx.doi.org/10.1002/qj.2010
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spelling crwiley:10.1002/qj.2010 2024-06-02T08:11:04+00:00 Observational evidence for the mechanism of the poleward propagation of zonal wind anomalies over the North Atlantic Yuan, Jiacan Lee, Sukyoung Tan, Benkui 2012 http://dx.doi.org/10.1002/qj.2010 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.2010 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.2010 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Quarterly Journal of the Royal Meteorological Society volume 139, issue 673, page 992-998 ISSN 0035-9009 1477-870X journal-article 2012 crwiley https://doi.org/10.1002/qj.2010 2024-05-03T11:06:05Z Abstract This study examines the physical mechanisms that drive the poleward propagation of zonal‐mean flow anomalies over the North Atlantic during the boreal winter with ECMWF ERA40 reanalysis data that spans the years 1958–2001. An empirical orthogonal function (EOF) analysis is performed on the zonal wind anomalies for the North Atlantic domain. Based on time‐lag correlations between the first two EOFs, 14 poleward propagation events are identified. A series of lagged composite calculations of the poleward propagation events reveals the following processes: midlatitude synoptic‐scale Rossby waves propagate equatorward and break when they encounter their critical latitudes in the Tropics and Subtropics; a new critical latitude is generated slightly poleward of the previous critical latitude, and the subsequent wave breaking occurs at this new critical latitude. This interaction between the wave breaking and the critical latitude drives the poleward propagation of zonal‐mean zonal wind anomaly. A comparison between the poleward propagation events and zonal index events indicates that the poleward propagation is associated with a relatively weak potential vorticity gradient over the Subtropics. These North Atlantic poleward propagation events are found to be preceded by anomalously strong transient eddy activity over the subtropical North Pacific, and by anomalously weak tropical convection over the tropical Atlantic Ocean and the Amazon. Copyright © 2012 Royal Meteorological Society Article in Journal/Newspaper North Atlantic Wiley Online Library Pacific Quarterly Journal of the Royal Meteorological Society 139 673 992 998
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract This study examines the physical mechanisms that drive the poleward propagation of zonal‐mean flow anomalies over the North Atlantic during the boreal winter with ECMWF ERA40 reanalysis data that spans the years 1958–2001. An empirical orthogonal function (EOF) analysis is performed on the zonal wind anomalies for the North Atlantic domain. Based on time‐lag correlations between the first two EOFs, 14 poleward propagation events are identified. A series of lagged composite calculations of the poleward propagation events reveals the following processes: midlatitude synoptic‐scale Rossby waves propagate equatorward and break when they encounter their critical latitudes in the Tropics and Subtropics; a new critical latitude is generated slightly poleward of the previous critical latitude, and the subsequent wave breaking occurs at this new critical latitude. This interaction between the wave breaking and the critical latitude drives the poleward propagation of zonal‐mean zonal wind anomaly. A comparison between the poleward propagation events and zonal index events indicates that the poleward propagation is associated with a relatively weak potential vorticity gradient over the Subtropics. These North Atlantic poleward propagation events are found to be preceded by anomalously strong transient eddy activity over the subtropical North Pacific, and by anomalously weak tropical convection over the tropical Atlantic Ocean and the Amazon. Copyright © 2012 Royal Meteorological Society
format Article in Journal/Newspaper
author Yuan, Jiacan
Lee, Sukyoung
Tan, Benkui
spellingShingle Yuan, Jiacan
Lee, Sukyoung
Tan, Benkui
Observational evidence for the mechanism of the poleward propagation of zonal wind anomalies over the North Atlantic
author_facet Yuan, Jiacan
Lee, Sukyoung
Tan, Benkui
author_sort Yuan, Jiacan
title Observational evidence for the mechanism of the poleward propagation of zonal wind anomalies over the North Atlantic
title_short Observational evidence for the mechanism of the poleward propagation of zonal wind anomalies over the North Atlantic
title_full Observational evidence for the mechanism of the poleward propagation of zonal wind anomalies over the North Atlantic
title_fullStr Observational evidence for the mechanism of the poleward propagation of zonal wind anomalies over the North Atlantic
title_full_unstemmed Observational evidence for the mechanism of the poleward propagation of zonal wind anomalies over the North Atlantic
title_sort observational evidence for the mechanism of the poleward propagation of zonal wind anomalies over the north atlantic
publisher Wiley
publishDate 2012
url http://dx.doi.org/10.1002/qj.2010
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.2010
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.2010
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_source Quarterly Journal of the Royal Meteorological Society
volume 139, issue 673, page 992-998
ISSN 0035-9009 1477-870X
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/qj.2010
container_title Quarterly Journal of the Royal Meteorological Society
container_volume 139
container_issue 673
container_start_page 992
op_container_end_page 998
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