Relative contributions of local heat storage and ocean heat transport to cold‐season Arctic Ocean surface energy fluxes in CMIP6 models

Abstract The Arctic near‐surface air temperature increases most strongly during the cold season, and ocean heat storage has often been cited as a crucial component in linking the ice‐albedo radiative feedback, which is active in summer, and near‐surface air temperature increase in winter, when the l...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Hajjar, Khaled al, Salzmann, Marc
Other Authors: Deutsche Forschungsgemeinschaft
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:http://dx.doi.org/10.1002/qj.4496
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4496
id crwiley:10.1002/qj.4496
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spelling crwiley:10.1002/qj.4496 2024-09-15T17:35:49+00:00 Relative contributions of local heat storage and ocean heat transport to cold‐season Arctic Ocean surface energy fluxes in CMIP6 models Hajjar, Khaled al Salzmann, Marc Deutsche Forschungsgemeinschaft 2023 http://dx.doi.org/10.1002/qj.4496 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4496 en eng Wiley http://creativecommons.org/licenses/by/4.0/ Quarterly Journal of the Royal Meteorological Society volume 149, issue 755, page 2091-2106 ISSN 0035-9009 1477-870X journal-article 2023 crwiley https://doi.org/10.1002/qj.4496 2024-07-11T04:36:07Z Abstract The Arctic near‐surface air temperature increases most strongly during the cold season, and ocean heat storage has often been cited as a crucial component in linking the ice‐albedo radiative feedback, which is active in summer, and near‐surface air temperature increase in winter, when the lapse rate feedback contributes to Arctic warming. Here, we first estimate how much local heat storage and ocean heat transport contribute to net surface energy fluxes on a seasonal scale in CMIP6 models. We then compare contributions in a base state under weak anthropogenic forcing to a near‐present‐day state in which significant Arctic amplification is simulated. Our analysis indicates that, in a few regions, ocean heat transport plays a larger role for cold‐season net surface energy fluxes compared with local heat storage. Analyzing differences between past and near‐present‐day conditions suggests that the lapse rate feedback, which mainly acts during the cold season in warm water inflow regions, may be more strongly influenced than previously thought by increased ocean heat transport from lower latitudes. Article in Journal/Newspaper albedo Arctic Ocean Wiley Online Library Quarterly Journal of the Royal Meteorological Society 149 755 2091 2106
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The Arctic near‐surface air temperature increases most strongly during the cold season, and ocean heat storage has often been cited as a crucial component in linking the ice‐albedo radiative feedback, which is active in summer, and near‐surface air temperature increase in winter, when the lapse rate feedback contributes to Arctic warming. Here, we first estimate how much local heat storage and ocean heat transport contribute to net surface energy fluxes on a seasonal scale in CMIP6 models. We then compare contributions in a base state under weak anthropogenic forcing to a near‐present‐day state in which significant Arctic amplification is simulated. Our analysis indicates that, in a few regions, ocean heat transport plays a larger role for cold‐season net surface energy fluxes compared with local heat storage. Analyzing differences between past and near‐present‐day conditions suggests that the lapse rate feedback, which mainly acts during the cold season in warm water inflow regions, may be more strongly influenced than previously thought by increased ocean heat transport from lower latitudes.
author2 Deutsche Forschungsgemeinschaft
format Article in Journal/Newspaper
author Hajjar, Khaled al
Salzmann, Marc
spellingShingle Hajjar, Khaled al
Salzmann, Marc
Relative contributions of local heat storage and ocean heat transport to cold‐season Arctic Ocean surface energy fluxes in CMIP6 models
author_facet Hajjar, Khaled al
Salzmann, Marc
author_sort Hajjar, Khaled al
title Relative contributions of local heat storage and ocean heat transport to cold‐season Arctic Ocean surface energy fluxes in CMIP6 models
title_short Relative contributions of local heat storage and ocean heat transport to cold‐season Arctic Ocean surface energy fluxes in CMIP6 models
title_full Relative contributions of local heat storage and ocean heat transport to cold‐season Arctic Ocean surface energy fluxes in CMIP6 models
title_fullStr Relative contributions of local heat storage and ocean heat transport to cold‐season Arctic Ocean surface energy fluxes in CMIP6 models
title_full_unstemmed Relative contributions of local heat storage and ocean heat transport to cold‐season Arctic Ocean surface energy fluxes in CMIP6 models
title_sort relative contributions of local heat storage and ocean heat transport to cold‐season arctic ocean surface energy fluxes in cmip6 models
publisher Wiley
publishDate 2023
url http://dx.doi.org/10.1002/qj.4496
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4496
genre albedo
Arctic Ocean
genre_facet albedo
Arctic Ocean
op_source Quarterly Journal of the Royal Meteorological Society
volume 149, issue 755, page 2091-2106
ISSN 0035-9009 1477-870X
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1002/qj.4496
container_title Quarterly Journal of the Royal Meteorological Society
container_volume 149
container_issue 755
container_start_page 2091
op_container_end_page 2106
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