The coupled atmosphere-ocean response to Antarctic sea-ice loss

Ayres, Holly C.; Screen, James A.; Blockley, Edward W.; Bracegirdle, Thomas J. ORCID: https://orcid.org/0000-0002-8868-4739. 2022 The coupled atmosphere-ocean response to Antarctic sea-ice loss. Journal of Climate, 35 (14). 4665-4685. 10.1175/JCLI-D-21-0918.1

Before downloading, please read NORA policies.

Preview

Text © Copyright 2022 American Meteorological Society (AMS). For permission to reuse any portion of this Work, please contact permissions@ametsoc.org. Any use of material in this Work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC § 108) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. All AMS journals and monograph publications are registered with the Copyright Clearance Center (https://www.copyright.com). Additional details are provided in the AMS Copyright Policy statement, available on the AMS website (https://www.ametsoc.org/PUBSCopyrightPolicy). clim-JCLI-D-21-0918.1.pdf - Published Version Download (4MB) | Preview

Text © 2022 American Meteorological Society. [15200442 - Journal of Climate] The coupled atmosphere-ocean response to Antarctic sea-ice loss.pdf - Accepted Version Restricted to NORA staff only Download (4MB) | Request a copy

Abstract/Summary

Antarctic sea ice is projected to decrease in response to increasing greenhouse gas concentrations. Limited studies so far have examined the coupled atmosphere-ocean response to Antarctic sea-ice loss. Here, we isolate the response to Antarctic sea-ice loss in the atmosphere and ocean using bespoke sea-ice albedo perturbation experiments with HadGEM3-GC31-LL, provide the first detailed examination of the global ocean response, and quantify the importance of atmosphere-ocean coupling, through comparison to uncoupled experiments with prescribed Antarctic sea-ice loss. Lower tropospheric warming and moistening over regions of sea-ice loss and the nearby Southern Ocean are simulated in both coupled and uncoupled configurations but are of greater magnitude in the coupled model. A weakening and equatorward shift of the tropospheric westerly jet are simulated in both configurations, but are also larger in the coupled model. Ocean coupling allows the warming response to spread northward, and by poleward atmospheric energy transport, back to the Antarctic interior. Warmer tropical sea surface temperatures enhance atmospheric convection, driving upper-tropospheric warming and triggering atmospheric teleconnections to the extratropics, including a weakened Aleutian Low. A 20% reduction in Antarctic Circumpolar Current transport and a weakening of the shallow tropical convergence cell are simulated. Surface waters warm and freshen globally, becoming more stratified and stable in the Southern Ocean, with similar changes, but of lesser magnitude, in the Arctic Ocean, where sea ice declines. Our results suggest that the climate effects of Antarctic sea-ice loss stretch from pole-to-pole and from the heights of the tropical troposphere to the depths of the Southern Ocean.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1175/JCLI-D-21-0918.1
ISSN:	0894-8755
Date made live:	03 May 2022 15:02 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/532577

Actions (login required)

View Item

Document Downloads

More statistics for this item...