Key roles for atmospheric feedback and mesoscale eddies in modelling the AMOC response to enhanced Greenland runoff ...

<!--!introduction!--> To understand and project the implications of enhanced Greenland Ice Sheet mass loss and potential Atlantic Meridional Overturning Circulation weakening it is necessary to determine and overcome challenges in simulating their complex linkages. We discuss the role of the o...

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Main Authors: Martin, Torge, Biastoch, Arne
Format: Conference Object
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-3852
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020693
id ftdatacite:10.57757/iugg23-3852
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spelling ftdatacite:10.57757/iugg23-3852 2023-07-23T04:19:27+02:00 Key roles for atmospheric feedback and mesoscale eddies in modelling the AMOC response to enhanced Greenland runoff ... Martin, Torge Biastoch, Arne 2023 https://dx.doi.org/10.57757/iugg23-3852 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020693 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Article ConferencePaper Oral 2023 ftdatacite https://doi.org/10.57757/iugg23-3852 2023-07-03T22:06:24Z <!--!introduction!--> To understand and project the implications of enhanced Greenland Ice Sheet mass loss and potential Atlantic Meridional Overturning Circulation weakening it is necessary to determine and overcome challenges in simulating their complex linkages. We discuss the role of the ocean mean state, subpolar gyre circulation, mesoscale eddies and atmospheric coupling in shaping the response of the subpolar North Atlantic Ocean to enhanced Greenland runoff. A suite of eight dedicated 60 to 100-year long model experiments with and without atmospheric coupling, with eddy processes parameterized and explicitly simulated, and with regular and significantly enlarged Greenland runoff is presented. The important role of an interactive atmosphere stands out as being crucial for limiting the AMOC weakening because its response to ocean changes enables a compensating temperature feedback. Further, explicitly simulating mesoscale dynamics yields a more realistic distribution path of the meltwater along ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Conference Object Greenland Ice Sheet North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Greenland
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description <!--!introduction!--> To understand and project the implications of enhanced Greenland Ice Sheet mass loss and potential Atlantic Meridional Overturning Circulation weakening it is necessary to determine and overcome challenges in simulating their complex linkages. We discuss the role of the ocean mean state, subpolar gyre circulation, mesoscale eddies and atmospheric coupling in shaping the response of the subpolar North Atlantic Ocean to enhanced Greenland runoff. A suite of eight dedicated 60 to 100-year long model experiments with and without atmospheric coupling, with eddy processes parameterized and explicitly simulated, and with regular and significantly enlarged Greenland runoff is presented. The important role of an interactive atmosphere stands out as being crucial for limiting the AMOC weakening because its response to ocean changes enables a compensating temperature feedback. Further, explicitly simulating mesoscale dynamics yields a more realistic distribution path of the meltwater along ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...
format Conference Object
author Martin, Torge
Biastoch, Arne
spellingShingle Martin, Torge
Biastoch, Arne
Key roles for atmospheric feedback and mesoscale eddies in modelling the AMOC response to enhanced Greenland runoff ...
author_facet Martin, Torge
Biastoch, Arne
author_sort Martin, Torge
title Key roles for atmospheric feedback and mesoscale eddies in modelling the AMOC response to enhanced Greenland runoff ...
title_short Key roles for atmospheric feedback and mesoscale eddies in modelling the AMOC response to enhanced Greenland runoff ...
title_full Key roles for atmospheric feedback and mesoscale eddies in modelling the AMOC response to enhanced Greenland runoff ...
title_fullStr Key roles for atmospheric feedback and mesoscale eddies in modelling the AMOC response to enhanced Greenland runoff ...
title_full_unstemmed Key roles for atmospheric feedback and mesoscale eddies in modelling the AMOC response to enhanced Greenland runoff ...
title_sort key roles for atmospheric feedback and mesoscale eddies in modelling the amoc response to enhanced greenland runoff ...
publisher GFZ German Research Centre for Geosciences
publishDate 2023
url https://dx.doi.org/10.57757/iugg23-3852
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020693
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
North Atlantic
genre_facet Greenland
Ice Sheet
North Atlantic
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.57757/iugg23-3852
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