Impact of sea spray‐mediated heat fluxes on polar low development

Abstract Sea spray, originating from wave breaking under high wind conditions, can significantly affect turbulent heat fluxes at the air–sea interface. Even though polar lows (PLs) can become extreme weather features with gale‐force wind, the impact of sea spray on their development has rarely been...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Lin, Ting, Spengler, Thomas, Rutgersson, Anna, Wu, Lichuan
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Online Access:http://dx.doi.org/10.1002/qj.4746
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4746
id crwiley:10.1002/qj.4746
record_format openpolar
spelling crwiley:10.1002/qj.4746 2024-09-15T17:57:58+00:00 Impact of sea spray‐mediated heat fluxes on polar low development Lin, Ting Spengler, Thomas Rutgersson, Anna Wu, Lichuan 2024 http://dx.doi.org/10.1002/qj.4746 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4746 en eng Wiley http://creativecommons.org/licenses/by/4.0/ Quarterly Journal of the Royal Meteorological Society volume 150, issue 762, page 2976-2990 ISSN 0035-9009 1477-870X journal-article 2024 crwiley https://doi.org/10.1002/qj.4746 2024-08-09T04:30:49Z Abstract Sea spray, originating from wave breaking under high wind conditions, can significantly affect turbulent heat fluxes at the air–sea interface. Even though polar lows (PLs) can become extreme weather features with gale‐force wind, the impact of sea spray on their development has rarely been investigated and is not considered in operational forecast models. In this study, the impact of sea spray on the development of two PLs over the Barents Sea is studied based on sensitivity experiments with an atmosphere–wave coupled model, where the spray‐mediated heat fluxes are parameterized. The results show that the impact of sea‐spray‐mediated heat fluxes on PL development is sensitive to the surface wind speed. In the case of the stronger PL, the higher surface wind speed results in significantly higher spray‐mediated heat fluxes. Consequently, these spray‐mediated heat fluxes intensify the convection and diabatic heating of the PL, resulting in its intensification. In comparison, the case with a weaker PL experiences less sea spray production and lower spray‐mediated heat fluxes due to its weaker surface wind speeds. Overall, we find that spray‐mediated sensible heat fluxes play an important role in the development of PLs, while the latent heat fluxes induced by sea spray have a relatively minor impact. Article in Journal/Newspaper Barents Sea Wiley Online Library Quarterly Journal of the Royal Meteorological Society 150 762 2976 2990
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Sea spray, originating from wave breaking under high wind conditions, can significantly affect turbulent heat fluxes at the air–sea interface. Even though polar lows (PLs) can become extreme weather features with gale‐force wind, the impact of sea spray on their development has rarely been investigated and is not considered in operational forecast models. In this study, the impact of sea spray on the development of two PLs over the Barents Sea is studied based on sensitivity experiments with an atmosphere–wave coupled model, where the spray‐mediated heat fluxes are parameterized. The results show that the impact of sea‐spray‐mediated heat fluxes on PL development is sensitive to the surface wind speed. In the case of the stronger PL, the higher surface wind speed results in significantly higher spray‐mediated heat fluxes. Consequently, these spray‐mediated heat fluxes intensify the convection and diabatic heating of the PL, resulting in its intensification. In comparison, the case with a weaker PL experiences less sea spray production and lower spray‐mediated heat fluxes due to its weaker surface wind speeds. Overall, we find that spray‐mediated sensible heat fluxes play an important role in the development of PLs, while the latent heat fluxes induced by sea spray have a relatively minor impact.
format Article in Journal/Newspaper
author Lin, Ting
Spengler, Thomas
Rutgersson, Anna
Wu, Lichuan
spellingShingle Lin, Ting
Spengler, Thomas
Rutgersson, Anna
Wu, Lichuan
Impact of sea spray‐mediated heat fluxes on polar low development
author_facet Lin, Ting
Spengler, Thomas
Rutgersson, Anna
Wu, Lichuan
author_sort Lin, Ting
title Impact of sea spray‐mediated heat fluxes on polar low development
title_short Impact of sea spray‐mediated heat fluxes on polar low development
title_full Impact of sea spray‐mediated heat fluxes on polar low development
title_fullStr Impact of sea spray‐mediated heat fluxes on polar low development
title_full_unstemmed Impact of sea spray‐mediated heat fluxes on polar low development
title_sort impact of sea spray‐mediated heat fluxes on polar low development
publisher Wiley
publishDate 2024
url http://dx.doi.org/10.1002/qj.4746
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.4746
genre Barents Sea
genre_facet Barents Sea
op_source Quarterly Journal of the Royal Meteorological Society
volume 150, issue 762, page 2976-2990
ISSN 0035-9009 1477-870X
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1002/qj.4746
container_title Quarterly Journal of the Royal Meteorological Society
container_volume 150
container_issue 762
container_start_page 2976
op_container_end_page 2990
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