Changes in the global heat transport and eddy‐mean flow interaction associated with weaker thermohaline circulation

Abstract This study investigates the anomalous patterns of the oceanic and atmospheric heat transport, transient waves and the interaction between transient waves and the mean zonal flow. The evaluation is based on simulations performed with a coupled model forced by an increase of 1 Sverdrup of fre...

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Published in:International Journal of Climatology
Main Authors: Machado, Jeferson Prietsch, Justino, Flavio, Pezzi, Luciano Ponzi
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2011
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.3411
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spelling crwiley:10.1002/joc.3411 2024-06-02T08:11:09+00:00 Changes in the global heat transport and eddy‐mean flow interaction associated with weaker thermohaline circulation Machado, Jeferson Prietsch Justino, Flavio Pezzi, Luciano Ponzi 2011 http://dx.doi.org/10.1002/joc.3411 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.3411 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.3411 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 32, issue 15, page 2255-2270 ISSN 0899-8418 1097-0088 journal-article 2011 crwiley https://doi.org/10.1002/joc.3411 2024-05-03T12:07:28Z Abstract This study investigates the anomalous patterns of the oceanic and atmospheric heat transport, transient waves and the interaction between transient waves and the mean zonal flow. The evaluation is based on simulations performed with a coupled model forced by an increase of 1 Sverdrup of freshwater flux into the North Atlantic Ocean. It is found that an increase of freshwater flux in the North Atlantic leads to a weakening in the Northern Hemisphere (NH) oceanic heat transport by up to 1 Petawatt (10 15 ) PW but results in an intensification of the Southern Hemisphere (SH) total heat transport. This inter‐hemispheric seesaw leads to substantial changes in transient wave activity which is associated with anomalous meridional temperature flux and eddy kinetic energy (EKE). During winter in the NH, weakening of the thermohaline circulation induces an increase in the storm track activity. However, a reduction in storm tracks is found over the extratropical regions of the SH. The correspondence between the anomalies of storm track intensity and Eady growth rate lead to the conclusion that changes in the transient eddy activity are mostly generated by changes in baroclinic conditions. Furthermore, calculations of the E vector show that interaction between transient and mean flow is most pronounced over the North Atlantic where stronger storm tracks enhance the mean westerlies, thus minimising the effect of changes in the oceanic heat transport. Copyright © 2011 Royal Meteorological Society Article in Journal/Newspaper North Atlantic Wiley Online Library International Journal of Climatology 32 15 2255 2270
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract This study investigates the anomalous patterns of the oceanic and atmospheric heat transport, transient waves and the interaction between transient waves and the mean zonal flow. The evaluation is based on simulations performed with a coupled model forced by an increase of 1 Sverdrup of freshwater flux into the North Atlantic Ocean. It is found that an increase of freshwater flux in the North Atlantic leads to a weakening in the Northern Hemisphere (NH) oceanic heat transport by up to 1 Petawatt (10 15 ) PW but results in an intensification of the Southern Hemisphere (SH) total heat transport. This inter‐hemispheric seesaw leads to substantial changes in transient wave activity which is associated with anomalous meridional temperature flux and eddy kinetic energy (EKE). During winter in the NH, weakening of the thermohaline circulation induces an increase in the storm track activity. However, a reduction in storm tracks is found over the extratropical regions of the SH. The correspondence between the anomalies of storm track intensity and Eady growth rate lead to the conclusion that changes in the transient eddy activity are mostly generated by changes in baroclinic conditions. Furthermore, calculations of the E vector show that interaction between transient and mean flow is most pronounced over the North Atlantic where stronger storm tracks enhance the mean westerlies, thus minimising the effect of changes in the oceanic heat transport. Copyright © 2011 Royal Meteorological Society
format Article in Journal/Newspaper
author Machado, Jeferson Prietsch
Justino, Flavio
Pezzi, Luciano Ponzi
spellingShingle Machado, Jeferson Prietsch
Justino, Flavio
Pezzi, Luciano Ponzi
Changes in the global heat transport and eddy‐mean flow interaction associated with weaker thermohaline circulation
author_facet Machado, Jeferson Prietsch
Justino, Flavio
Pezzi, Luciano Ponzi
author_sort Machado, Jeferson Prietsch
title Changes in the global heat transport and eddy‐mean flow interaction associated with weaker thermohaline circulation
title_short Changes in the global heat transport and eddy‐mean flow interaction associated with weaker thermohaline circulation
title_full Changes in the global heat transport and eddy‐mean flow interaction associated with weaker thermohaline circulation
title_fullStr Changes in the global heat transport and eddy‐mean flow interaction associated with weaker thermohaline circulation
title_full_unstemmed Changes in the global heat transport and eddy‐mean flow interaction associated with weaker thermohaline circulation
title_sort changes in the global heat transport and eddy‐mean flow interaction associated with weaker thermohaline circulation
publisher Wiley
publishDate 2011
url http://dx.doi.org/10.1002/joc.3411
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.3411
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.3411
genre North Atlantic
genre_facet North Atlantic
op_source International Journal of Climatology
volume 32, issue 15, page 2255-2270
ISSN 0899-8418 1097-0088
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/joc.3411
container_title International Journal of Climatology
container_volume 32
container_issue 15
container_start_page 2255
op_container_end_page 2270
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