Southern Ocean heat storage, reemergence, and winter sea ice decline induced by summertime winds
Ó 2021 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy The observational record shows a substantial 40-yr upward trend in summertime westerly winds over the Southern Ocean, as characterized by the so...
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ftmit:oai:dspace.mit.edu:1721.1/133818.2 2023-06-11T04:16:31+02:00 Southern Ocean heat storage, reemergence, and winter sea ice decline induced by summertime winds Doddridge, Edward W Marshall, John Song, Hajoon Campin, Jean-Michel Kelley, Maxwell 2021-09-17T13:48:37Z application/octet-stream https://hdl.handle.net/1721.1/133818.2 en eng American Meteorological Society http://dx.doi.org/10.1175/JCLI-D-20-0322.1 Journal of Climate 0894-8755 1520-0442 https://hdl.handle.net/1721.1/133818.2 Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. American Meteorological Society (AMS) Article http://purl.org/eprint/type/JournalArticle 2021 ftmit https://doi.org/10.1175/JCLI-D-20-0322.1 2023-05-29T08:51:14Z Ó 2021 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy The observational record shows a substantial 40-yr upward trend in summertime westerly winds over the Southern Ocean, as characterized by the southern annular mode (SAM) index. Enhanced summertime westerly winds have been linked to cold summertime sea surface temperature (SST) anomalies. Previous studies have suggested that Ekman transport or upwelling is responsible for this seasonal cooling. Here, another process is presented in which enhanced vertical mixing, driven by summertime wind anomalies, moves heat downward, cooling the sea surface and simultaneously warming the subsurface waters. The anomalously cold SSTs draw heat from the atmosphere into the ocean, leading to increased depth-integrated ocean heat content. The subsurface heat is returned to the surface mixed layer during the autumn and winter as the mixed layer deepens, leading to anomalously warm SSTs and potentially reducing sea ice cover. Observational analyses and numerical experiments support our proposed mechanism, showing that enhanced vertical mixing produces subsurface warming and cools the surface mixed layer. Nevertheless, the dominant driver of surface cooling remains uncertain; the relative importance of advective and mixing contributions to the surface cooling is model dependent. Modeling results suggest that sea ice volume is more sensitive to summertime winds than sea ice extent, implying that enhanced summertime westerly winds may lead to thinner sea ice in the following winter, if not lesser ice extent. Thus, strong summertime winds could precondition the sea ice cover for a rapid retreat in the following melt season. Article in Journal/Newspaper Sea ice Southern Ocean DSpace@MIT (Massachusetts Institute of Technology) Southern Ocean Journal of Climate 34 4 1403 1415 |
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English |
description |
Ó 2021 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy The observational record shows a substantial 40-yr upward trend in summertime westerly winds over the Southern Ocean, as characterized by the southern annular mode (SAM) index. Enhanced summertime westerly winds have been linked to cold summertime sea surface temperature (SST) anomalies. Previous studies have suggested that Ekman transport or upwelling is responsible for this seasonal cooling. Here, another process is presented in which enhanced vertical mixing, driven by summertime wind anomalies, moves heat downward, cooling the sea surface and simultaneously warming the subsurface waters. The anomalously cold SSTs draw heat from the atmosphere into the ocean, leading to increased depth-integrated ocean heat content. The subsurface heat is returned to the surface mixed layer during the autumn and winter as the mixed layer deepens, leading to anomalously warm SSTs and potentially reducing sea ice cover. Observational analyses and numerical experiments support our proposed mechanism, showing that enhanced vertical mixing produces subsurface warming and cools the surface mixed layer. Nevertheless, the dominant driver of surface cooling remains uncertain; the relative importance of advective and mixing contributions to the surface cooling is model dependent. Modeling results suggest that sea ice volume is more sensitive to summertime winds than sea ice extent, implying that enhanced summertime westerly winds may lead to thinner sea ice in the following winter, if not lesser ice extent. Thus, strong summertime winds could precondition the sea ice cover for a rapid retreat in the following melt season. |
format |
Article in Journal/Newspaper |
author |
Doddridge, Edward W Marshall, John Song, Hajoon Campin, Jean-Michel Kelley, Maxwell |
spellingShingle |
Doddridge, Edward W Marshall, John Song, Hajoon Campin, Jean-Michel Kelley, Maxwell Southern Ocean heat storage, reemergence, and winter sea ice decline induced by summertime winds |
author_facet |
Doddridge, Edward W Marshall, John Song, Hajoon Campin, Jean-Michel Kelley, Maxwell |
author_sort |
Doddridge, Edward W |
title |
Southern Ocean heat storage, reemergence, and winter sea ice decline induced by summertime winds |
title_short |
Southern Ocean heat storage, reemergence, and winter sea ice decline induced by summertime winds |
title_full |
Southern Ocean heat storage, reemergence, and winter sea ice decline induced by summertime winds |
title_fullStr |
Southern Ocean heat storage, reemergence, and winter sea ice decline induced by summertime winds |
title_full_unstemmed |
Southern Ocean heat storage, reemergence, and winter sea ice decline induced by summertime winds |
title_sort |
southern ocean heat storage, reemergence, and winter sea ice decline induced by summertime winds |
publisher |
American Meteorological Society |
publishDate |
2021 |
url |
https://hdl.handle.net/1721.1/133818.2 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Sea ice Southern Ocean |
genre_facet |
Sea ice Southern Ocean |
op_source |
American Meteorological Society (AMS) |
op_relation |
http://dx.doi.org/10.1175/JCLI-D-20-0322.1 Journal of Climate 0894-8755 1520-0442 https://hdl.handle.net/1721.1/133818.2 |
op_rights |
Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. |
op_doi |
https://doi.org/10.1175/JCLI-D-20-0322.1 |
container_title |
Journal of Climate |
container_volume |
34 |
container_issue |
4 |
container_start_page |
1403 |
op_container_end_page |
1415 |
_version_ |
1768374854617137152 |