Sea‐Ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate ...

Much of the Southern Ocean surface south of 55° S cooled and freshened between at least the early 1980s and the early 2010s. Many processes have been proposed to explain the unexpected cooling, including increased winds or freshwater fluxes. However, these mechanisms so far failed to fully explain t...

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Main Authors: Haumann, Alexander, Gruber, Nicolas, Münnich, Matthias
Format: Article in Journal/Newspaper
Language:English
Published: ETH Zurich 2020
Subjects:
Online Access:https://dx.doi.org/10.3929/ethz-b-000415934
http://hdl.handle.net/20.500.11850/415934
id ftdatacite:10.3929/ethz-b-000415934
record_format openpolar
spelling ftdatacite:10.3929/ethz-b-000415934 2024-04-28T07:56:21+00:00 Sea‐Ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate ... Haumann, Alexander Gruber, Nicolas Münnich, Matthias 2020 application/pdf https://dx.doi.org/10.3929/ethz-b-000415934 http://hdl.handle.net/20.500.11850/415934 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 Southern Ocean sea ice glacial meltwater cooling warming freshwater article-journal Text ScholarlyArticle Journal Article 2020 ftdatacite https://doi.org/10.3929/ethz-b-000415934 2024-04-02T12:34:54Z Much of the Southern Ocean surface south of 55° S cooled and freshened between at least the early 1980s and the early 2010s. Many processes have been proposed to explain the unexpected cooling, including increased winds or freshwater fluxes. However, these mechanisms so far failed to fully explain the surface trends and the concurrent subsurface warming (100 to 500 m). Here, we argue that these trends are predominantly caused by an increased wind‐driven northward sea‐ice transport, enhancing the extraction of freshwater near Antarctica and releasing it in the open ocean. This conclusion is based on factorial experiments with a regional ocean model. In all experiments with an enhanced northward sea‐ice transport, a strengthened salinity‐dominated stratification cools the open‐ocean surface waters between the Subantarctic Front and the sea‐ice edge. The strengthened stratification reduces the downward mixing of cold surface water and the upward heat loss of the warmer waters below, thus warming the subsurface. ... : AGU Advances, 1 (2) ... Article in Journal/Newspaper Antarc* Antarctica Sea ice Southern Ocean DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Southern Ocean
sea ice
glacial meltwater
cooling
warming
freshwater
spellingShingle Southern Ocean
sea ice
glacial meltwater
cooling
warming
freshwater
Haumann, Alexander
Gruber, Nicolas
Münnich, Matthias
Sea‐Ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate ...
topic_facet Southern Ocean
sea ice
glacial meltwater
cooling
warming
freshwater
description Much of the Southern Ocean surface south of 55° S cooled and freshened between at least the early 1980s and the early 2010s. Many processes have been proposed to explain the unexpected cooling, including increased winds or freshwater fluxes. However, these mechanisms so far failed to fully explain the surface trends and the concurrent subsurface warming (100 to 500 m). Here, we argue that these trends are predominantly caused by an increased wind‐driven northward sea‐ice transport, enhancing the extraction of freshwater near Antarctica and releasing it in the open ocean. This conclusion is based on factorial experiments with a regional ocean model. In all experiments with an enhanced northward sea‐ice transport, a strengthened salinity‐dominated stratification cools the open‐ocean surface waters between the Subantarctic Front and the sea‐ice edge. The strengthened stratification reduces the downward mixing of cold surface water and the upward heat loss of the warmer waters below, thus warming the subsurface. ... : AGU Advances, 1 (2) ...
format Article in Journal/Newspaper
author Haumann, Alexander
Gruber, Nicolas
Münnich, Matthias
author_facet Haumann, Alexander
Gruber, Nicolas
Münnich, Matthias
author_sort Haumann, Alexander
title Sea‐Ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate ...
title_short Sea‐Ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate ...
title_full Sea‐Ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate ...
title_fullStr Sea‐Ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate ...
title_full_unstemmed Sea‐Ice Induced Southern Ocean Subsurface Warming and Surface Cooling in a Warming Climate ...
title_sort sea‐ice induced southern ocean subsurface warming and surface cooling in a warming climate ...
publisher ETH Zurich
publishDate 2020
url https://dx.doi.org/10.3929/ethz-b-000415934
http://hdl.handle.net/20.500.11850/415934
genre Antarc*
Antarctica
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctica
Sea ice
Southern Ocean
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution Non Commercial No Derivatives 4.0 International
https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
cc-by-nc-nd-4.0
op_doi https://doi.org/10.3929/ethz-b-000415934
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