Driving Mechanisms of an Extreme Winter Sea Ice Breakup Event in the Beaufort Sea

International audience Arctic sea ice is thinning (Meier, 2017) in conjunction with the decrease in the area covered by thick multiyear ice (MYI) (Kwok, 2018), which is replaced by thinner first-year ice (FYI) that is more mobile and less dynamically stable (Rampal et al., 2009; J. Zhang et al., 201...

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Published in:Geophysical Research Letters
Main Authors: Rheinlænder, Jonathan, W, Davy, Richard, Ólason, Einar, Rampal, Pierre, Spensberger, Clemens, Williams, Timothy, D, Korosov, Anton, Spengler, Thomas
Other Authors: Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2022
Subjects:
Online Access:https://hal.science/hal-03796513
https://hal.science/hal-03796513/document
https://hal.science/hal-03796513/file/Rheinl%C3%A6nder2022Geophsy._Res._Lett.pdf
https://doi.org/10.1029/2022gl099024
id ftunigrenoble:oai:HAL:hal-03796513v1
record_format openpolar
spelling ftunigrenoble:oai:HAL:hal-03796513v1 2024-05-12T07:59:06+00:00 Driving Mechanisms of an Extreme Winter Sea Ice Breakup Event in the Beaufort Sea Rheinlænder, Jonathan, W Davy, Richard Ólason, Einar Rampal, Pierre Spensberger, Clemens Williams, Timothy, D Korosov, Anton Spengler, Thomas Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) 2022-06-21 https://hal.science/hal-03796513 https://hal.science/hal-03796513/document https://hal.science/hal-03796513/file/Rheinl%C3%A6nder2022Geophsy._Res._Lett.pdf https://doi.org/10.1029/2022gl099024 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2022gl099024 hal-03796513 https://hal.science/hal-03796513 https://hal.science/hal-03796513/document https://hal.science/hal-03796513/file/Rheinl%C3%A6nder2022Geophsy._Res._Lett.pdf doi:10.1029/2022gl099024 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.science/hal-03796513 Geophysical Research Letters, 2022, 49, ⟨10.1029/2022gl099024⟩ [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2022 ftunigrenoble https://doi.org/10.1029/2022gl099024 2024-04-18T03:01:39Z International audience Arctic sea ice is thinning (Meier, 2017) in conjunction with the decrease in the area covered by thick multiyear ice (MYI) (Kwok, 2018), which is replaced by thinner first-year ice (FYI) that is more mobile and less dynamically stable (Rampal et al., 2009; J. Zhang et al., 2012). This makes the ice cover more vulnerable to intense winds breaking up the sea ice. In the Beaufort Sea in particular, the loss of MYI may contribute to the earlier onset of the melt season in recent years (Johnson & Eicken, 2016). When sea ice breaks up, it exposes the underlying warmer ocean within narrow, linear openings in the ice cover known as leads. This has important consequences for air-sea exchange, ocean eddy generation and dynamics, sea ice production, and Arctic Ocean properties in general (Cohanim et al., 2021; Graham et al., 2019; Nguyen et al., 2009), especially during the winter months when heat fluxes over sea ice are generally small (Andreas & Cash, 1999). In addition, breakup in winter weakens the ice cover, potentially preconditioning the minimum ice extent in summer (Y. Zhang et al., 2018; Babb et al., 2019) and thus creating a positive feedback to Arctic amplification (Dai et al., 2019). Therefore, extreme breakup events are of crucial interest for understanding the seasonal and long-term evolution of Arctic sea ice, which in turn affect weather, ecosystems, and local communities in polar regions and beyond (Forbes et al., 2016; Vihma, 2014). Article in Journal/Newspaper Arctic Arctic Ocean Beaufort Sea Sea ice Université Grenoble Alpes: HAL Andreas ENVELOPE(-60.729,-60.729,-64.008,-64.008) Arctic Arctic Ocean Forbes ENVELOPE(-66.550,-66.550,-67.783,-67.783) Meier ENVELOPE(-45.900,-45.900,-60.633,-60.633) Geophysical Research Letters 49 12
institution Open Polar
collection Université Grenoble Alpes: HAL
op_collection_id ftunigrenoble
language English
topic [SDE]Environmental Sciences
spellingShingle [SDE]Environmental Sciences
Rheinlænder, Jonathan, W
Davy, Richard
Ólason, Einar
Rampal, Pierre
Spensberger, Clemens
Williams, Timothy, D
Korosov, Anton
Spengler, Thomas
Driving Mechanisms of an Extreme Winter Sea Ice Breakup Event in the Beaufort Sea
topic_facet [SDE]Environmental Sciences
description International audience Arctic sea ice is thinning (Meier, 2017) in conjunction with the decrease in the area covered by thick multiyear ice (MYI) (Kwok, 2018), which is replaced by thinner first-year ice (FYI) that is more mobile and less dynamically stable (Rampal et al., 2009; J. Zhang et al., 2012). This makes the ice cover more vulnerable to intense winds breaking up the sea ice. In the Beaufort Sea in particular, the loss of MYI may contribute to the earlier onset of the melt season in recent years (Johnson & Eicken, 2016). When sea ice breaks up, it exposes the underlying warmer ocean within narrow, linear openings in the ice cover known as leads. This has important consequences for air-sea exchange, ocean eddy generation and dynamics, sea ice production, and Arctic Ocean properties in general (Cohanim et al., 2021; Graham et al., 2019; Nguyen et al., 2009), especially during the winter months when heat fluxes over sea ice are generally small (Andreas & Cash, 1999). In addition, breakup in winter weakens the ice cover, potentially preconditioning the minimum ice extent in summer (Y. Zhang et al., 2018; Babb et al., 2019) and thus creating a positive feedback to Arctic amplification (Dai et al., 2019). Therefore, extreme breakup events are of crucial interest for understanding the seasonal and long-term evolution of Arctic sea ice, which in turn affect weather, ecosystems, and local communities in polar regions and beyond (Forbes et al., 2016; Vihma, 2014).
author2 Institut des Géosciences de l’Environnement (IGE)
Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )
Université Grenoble Alpes (UGA)
format Article in Journal/Newspaper
author Rheinlænder, Jonathan, W
Davy, Richard
Ólason, Einar
Rampal, Pierre
Spensberger, Clemens
Williams, Timothy, D
Korosov, Anton
Spengler, Thomas
author_facet Rheinlænder, Jonathan, W
Davy, Richard
Ólason, Einar
Rampal, Pierre
Spensberger, Clemens
Williams, Timothy, D
Korosov, Anton
Spengler, Thomas
author_sort Rheinlænder, Jonathan, W
title Driving Mechanisms of an Extreme Winter Sea Ice Breakup Event in the Beaufort Sea
title_short Driving Mechanisms of an Extreme Winter Sea Ice Breakup Event in the Beaufort Sea
title_full Driving Mechanisms of an Extreme Winter Sea Ice Breakup Event in the Beaufort Sea
title_fullStr Driving Mechanisms of an Extreme Winter Sea Ice Breakup Event in the Beaufort Sea
title_full_unstemmed Driving Mechanisms of an Extreme Winter Sea Ice Breakup Event in the Beaufort Sea
title_sort driving mechanisms of an extreme winter sea ice breakup event in the beaufort sea
publisher HAL CCSD
publishDate 2022
url https://hal.science/hal-03796513
https://hal.science/hal-03796513/document
https://hal.science/hal-03796513/file/Rheinl%C3%A6nder2022Geophsy._Res._Lett.pdf
https://doi.org/10.1029/2022gl099024
long_lat ENVELOPE(-60.729,-60.729,-64.008,-64.008)
ENVELOPE(-66.550,-66.550,-67.783,-67.783)
ENVELOPE(-45.900,-45.900,-60.633,-60.633)
geographic Andreas
Arctic
Arctic Ocean
Forbes
Meier
geographic_facet Andreas
Arctic
Arctic Ocean
Forbes
Meier
genre Arctic
Arctic Ocean
Beaufort Sea
Sea ice
genre_facet Arctic
Arctic Ocean
Beaufort Sea
Sea ice
op_source ISSN: 0094-8276
EISSN: 1944-8007
Geophysical Research Letters
https://hal.science/hal-03796513
Geophysical Research Letters, 2022, 49, ⟨10.1029/2022gl099024⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2022gl099024
hal-03796513
https://hal.science/hal-03796513
https://hal.science/hal-03796513/document
https://hal.science/hal-03796513/file/Rheinl%C3%A6nder2022Geophsy._Res._Lett.pdf
doi:10.1029/2022gl099024
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2022gl099024
container_title Geophysical Research Letters
container_volume 49
container_issue 12
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