Feedbacks between ice cover, ocean stratification, and heat content in Ryder Bay, western Antarctic Peninsula

A multi-year, all-season time series of water column physical properties and sea ice conditions in Ryder Bay, at the western Antarctic Peninsula (WAP), is used to assess the effects on the ocean of varying ice cover. Reduced ice cover leads to increased mixing and heat loss in the winter. The reduct...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Venables, Hugh, Meredith, Michael
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2014
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/503955/
https://nora.nerc.ac.uk/id/eprint/503955/1/jgrc20834.pdf
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2013JC009669
id ftnerc:oai:nora.nerc.ac.uk:503955
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spelling ftnerc:oai:nora.nerc.ac.uk:503955 2023-05-15T13:48:08+02:00 Feedbacks between ice cover, ocean stratification, and heat content in Ryder Bay, western Antarctic Peninsula Venables, Hugh Meredith, Michael 2014-08-04 text http://nora.nerc.ac.uk/id/eprint/503955/ https://nora.nerc.ac.uk/id/eprint/503955/1/jgrc20834.pdf https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2013JC009669 en eng American Geophysical Union https://nora.nerc.ac.uk/id/eprint/503955/1/jgrc20834.pdf Venables, Hugh; Meredith, Michael orcid:0000-0002-7342-7756 . 2014 Feedbacks between ice cover, ocean stratification, and heat content in Ryder Bay, western Antarctic Peninsula. Journal of Geophysical Research: Oceans, 119 (8). 5323-5336. https://doi.org/10.1002/2013JC009669 <https://doi.org/10.1002/2013JC009669> Publication - Article PeerReviewed 2014 ftnerc https://doi.org/10.1002/2013JC009669 2023-02-04T19:38:10Z A multi-year, all-season time series of water column physical properties and sea ice conditions in Ryder Bay, at the western Antarctic Peninsula (WAP), is used to assess the effects on the ocean of varying ice cover. Reduced ice cover leads to increased mixing and heat loss in the winter. The reduction in stratification persists into the following summer, preconditioning the water column to a greater vertical extent of surface-driven mixing. This leads to an increased amount of heat from insolation being mixed down, affecting approximately the top 100m. The increased heat uptake in summer exceeds the heat lost the preceding winter, giving the initially counter-intuitive effect that enhanced winter cooling generates warmer temperatures in the following summer and autumn. This process is therefore a positive feedback on sea ice, as reduced sea ice leads to increased heat content in the ocean the following autumn. It also causes increased winter atmospheric temperatures due to the increased winter heat loss from the ocean. In the deeper part of the water column, heat and carbon stored in the Circumpolar Deep Water (CDW) layer are released by deep mixing events. At these depths, conditions are restored by advection and vertical mixing on multi-year timescales. In recent years, stronger deep mixing events in winter have led to a persistent reduction in CDW temperatures at the study site. Ocean glider data demonstrate the representativeness of these results across the wider region of Marguerite Bay, within which Ryder Bay is situated. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Sea ice Natural Environment Research Council: NERC Open Research Archive Antarctic Antarctic Peninsula Marguerite ENVELOPE(141.378,141.378,-66.787,-66.787) Marguerite Bay ENVELOPE(-68.000,-68.000,-68.500,-68.500) Ryder ENVELOPE(-68.333,-68.333,-67.566,-67.566) Ryder Bay ENVELOPE(-68.333,-68.333,-67.567,-67.567) Journal of Geophysical Research: Oceans 119 8 5323 5336
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
description A multi-year, all-season time series of water column physical properties and sea ice conditions in Ryder Bay, at the western Antarctic Peninsula (WAP), is used to assess the effects on the ocean of varying ice cover. Reduced ice cover leads to increased mixing and heat loss in the winter. The reduction in stratification persists into the following summer, preconditioning the water column to a greater vertical extent of surface-driven mixing. This leads to an increased amount of heat from insolation being mixed down, affecting approximately the top 100m. The increased heat uptake in summer exceeds the heat lost the preceding winter, giving the initially counter-intuitive effect that enhanced winter cooling generates warmer temperatures in the following summer and autumn. This process is therefore a positive feedback on sea ice, as reduced sea ice leads to increased heat content in the ocean the following autumn. It also causes increased winter atmospheric temperatures due to the increased winter heat loss from the ocean. In the deeper part of the water column, heat and carbon stored in the Circumpolar Deep Water (CDW) layer are released by deep mixing events. At these depths, conditions are restored by advection and vertical mixing on multi-year timescales. In recent years, stronger deep mixing events in winter have led to a persistent reduction in CDW temperatures at the study site. Ocean glider data demonstrate the representativeness of these results across the wider region of Marguerite Bay, within which Ryder Bay is situated.
format Article in Journal/Newspaper
author Venables, Hugh
Meredith, Michael
spellingShingle Venables, Hugh
Meredith, Michael
Feedbacks between ice cover, ocean stratification, and heat content in Ryder Bay, western Antarctic Peninsula
author_facet Venables, Hugh
Meredith, Michael
author_sort Venables, Hugh
title Feedbacks between ice cover, ocean stratification, and heat content in Ryder Bay, western Antarctic Peninsula
title_short Feedbacks between ice cover, ocean stratification, and heat content in Ryder Bay, western Antarctic Peninsula
title_full Feedbacks between ice cover, ocean stratification, and heat content in Ryder Bay, western Antarctic Peninsula
title_fullStr Feedbacks between ice cover, ocean stratification, and heat content in Ryder Bay, western Antarctic Peninsula
title_full_unstemmed Feedbacks between ice cover, ocean stratification, and heat content in Ryder Bay, western Antarctic Peninsula
title_sort feedbacks between ice cover, ocean stratification, and heat content in ryder bay, western antarctic peninsula
publisher American Geophysical Union
publishDate 2014
url http://nora.nerc.ac.uk/id/eprint/503955/
https://nora.nerc.ac.uk/id/eprint/503955/1/jgrc20834.pdf
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2013JC009669
long_lat ENVELOPE(141.378,141.378,-66.787,-66.787)
ENVELOPE(-68.000,-68.000,-68.500,-68.500)
ENVELOPE(-68.333,-68.333,-67.566,-67.566)
ENVELOPE(-68.333,-68.333,-67.567,-67.567)
geographic Antarctic
Antarctic Peninsula
Marguerite
Marguerite Bay
Ryder
Ryder Bay
geographic_facet Antarctic
Antarctic Peninsula
Marguerite
Marguerite Bay
Ryder
Ryder Bay
genre Antarc*
Antarctic
Antarctic Peninsula
Sea ice
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Sea ice
op_relation https://nora.nerc.ac.uk/id/eprint/503955/1/jgrc20834.pdf
Venables, Hugh; Meredith, Michael orcid:0000-0002-7342-7756 . 2014 Feedbacks between ice cover, ocean stratification, and heat content in Ryder Bay, western Antarctic Peninsula. Journal of Geophysical Research: Oceans, 119 (8). 5323-5336. https://doi.org/10.1002/2013JC009669 <https://doi.org/10.1002/2013JC009669>
op_doi https://doi.org/10.1002/2013JC009669
container_title Journal of Geophysical Research: Oceans
container_volume 119
container_issue 8
container_start_page 5323
op_container_end_page 5336
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