Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals

Polar regions are particularly sensitive to climate change, with the potential for significant feedbacks between ocean circulation, sea ice, and the ocean carbon cycle. However, the difficulty in obtaining in situ data means that our ability to detect and interpret change is very limited, especially...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: Charrassin, J.-B., Hindell, M., Rintoul, S.R., Roquet, F., Sokolov, S., Biuw, M., Costa, D., Boehme, L., Lovell, P., Coleman, R., Timmerman, R., Meijers, A., Meredith, M., Park, Y.-H., Bailleul, F., Goebel, M., Tremblay, Y., Bost, C.-A., McMahon, C., Field, I.C., Fedak, M.A., Guinet, C.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2008
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/5705/
https://doi.org/10.1073/pnas.0800790105
id ftnerc:oai:nora.nerc.ac.uk:5705
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spelling ftnerc:oai:nora.nerc.ac.uk:5705 2024-06-09T07:45:42+00:00 Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals Charrassin, J.-B. Hindell, M. Rintoul, S.R. Roquet, F. Sokolov, S. Biuw, M. Costa, D. Boehme, L. Lovell, P. Coleman, R. Timmerman, R. Meijers, A. Meredith, M. Park, Y.-H. Bailleul, F. Goebel, M. Tremblay, Y. Bost, C.-A. McMahon, C. Field, I.C. Fedak, M.A. Guinet, C. 2008 http://nora.nerc.ac.uk/id/eprint/5705/ https://doi.org/10.1073/pnas.0800790105 unknown Charrassin, J.-B.; Hindell, M.; Rintoul, S.R.; Roquet, F.; Sokolov, S.; Biuw, M.; Costa, D.; Boehme, L.; Lovell, P.; Coleman, R.; Timmerman, R.; Meijers, A.; Meredith, M. orcid:0000-0002-7342-7756 Park, Y.-H.; Bailleul, F.; Goebel, M.; Tremblay, Y.; Bost, C.-A.; McMahon, C.; Field, I.C.; Fedak, M.A.; Guinet, C. 2008 Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals. Proceedings of the National Academy of Sciences, 105 (33), Proceedings of the National Academy of Sciences. 11,634-11,639. https://doi.org/10.1073/pnas.0800790105 <https://doi.org/10.1073/pnas.0800790105> Marine Sciences Zoology Publication - Article PeerReviewed 2008 ftnerc https://doi.org/10.1073/pnas.0800790105 2024-05-15T08:49:44Z Polar regions are particularly sensitive to climate change, with the potential for significant feedbacks between ocean circulation, sea ice, and the ocean carbon cycle. However, the difficulty in obtaining in situ data means that our ability to detect and interpret change is very limited, especially in the Southern Ocean, where the ocean beneath the sea ice remains almost entirely unobserved and the rate of sea-ice formation is poorly known. Here, we show that southern elephant seals (Mirounga leonina) equipped with oceanographic sensors can measure ocean structure and water mass changes in regions and seasons rarely observed with traditional oceanographic platforms. In particular, seals provided a 30-fold increase in hydrographic profiles from the sea-ice zone, allowing the major fronts to be mapped south of 60°S and sea-ice formation rates to be inferred from changes in upper ocean salinity. Sea-ice production rates peaked in early winter (April–May) during the rapid northward expansion of the pack ice and declined by a factor of 2 to 3 between May and August, in agreement with a three dimensional coupled ocean–sea-ice model. By measuring the high latitude ocean during winter, elephant seals fill a ‘‘blind spot’’ in our sampling coverage, enabling the establishment of a truly global ocean-observing system. Article in Journal/Newspaper Elephant Seals Mirounga leonina Sea ice Southern Elephant Seals Southern Ocean Natural Environment Research Council: NERC Open Research Archive Southern Ocean Proceedings of the National Academy of Sciences 105 33 11634 11639
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
topic Marine Sciences
Zoology
spellingShingle Marine Sciences
Zoology
Charrassin, J.-B.
Hindell, M.
Rintoul, S.R.
Roquet, F.
Sokolov, S.
Biuw, M.
Costa, D.
Boehme, L.
Lovell, P.
Coleman, R.
Timmerman, R.
Meijers, A.
Meredith, M.
Park, Y.-H.
Bailleul, F.
Goebel, M.
Tremblay, Y.
Bost, C.-A.
McMahon, C.
Field, I.C.
Fedak, M.A.
Guinet, C.
Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals
topic_facet Marine Sciences
Zoology
description Polar regions are particularly sensitive to climate change, with the potential for significant feedbacks between ocean circulation, sea ice, and the ocean carbon cycle. However, the difficulty in obtaining in situ data means that our ability to detect and interpret change is very limited, especially in the Southern Ocean, where the ocean beneath the sea ice remains almost entirely unobserved and the rate of sea-ice formation is poorly known. Here, we show that southern elephant seals (Mirounga leonina) equipped with oceanographic sensors can measure ocean structure and water mass changes in regions and seasons rarely observed with traditional oceanographic platforms. In particular, seals provided a 30-fold increase in hydrographic profiles from the sea-ice zone, allowing the major fronts to be mapped south of 60°S and sea-ice formation rates to be inferred from changes in upper ocean salinity. Sea-ice production rates peaked in early winter (April–May) during the rapid northward expansion of the pack ice and declined by a factor of 2 to 3 between May and August, in agreement with a three dimensional coupled ocean–sea-ice model. By measuring the high latitude ocean during winter, elephant seals fill a ‘‘blind spot’’ in our sampling coverage, enabling the establishment of a truly global ocean-observing system.
format Article in Journal/Newspaper
author Charrassin, J.-B.
Hindell, M.
Rintoul, S.R.
Roquet, F.
Sokolov, S.
Biuw, M.
Costa, D.
Boehme, L.
Lovell, P.
Coleman, R.
Timmerman, R.
Meijers, A.
Meredith, M.
Park, Y.-H.
Bailleul, F.
Goebel, M.
Tremblay, Y.
Bost, C.-A.
McMahon, C.
Field, I.C.
Fedak, M.A.
Guinet, C.
author_facet Charrassin, J.-B.
Hindell, M.
Rintoul, S.R.
Roquet, F.
Sokolov, S.
Biuw, M.
Costa, D.
Boehme, L.
Lovell, P.
Coleman, R.
Timmerman, R.
Meijers, A.
Meredith, M.
Park, Y.-H.
Bailleul, F.
Goebel, M.
Tremblay, Y.
Bost, C.-A.
McMahon, C.
Field, I.C.
Fedak, M.A.
Guinet, C.
author_sort Charrassin, J.-B.
title Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals
title_short Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals
title_full Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals
title_fullStr Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals
title_full_unstemmed Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals
title_sort southern ocean frontal structure and sea ice formation rates revealed by elephant seals
publishDate 2008
url http://nora.nerc.ac.uk/id/eprint/5705/
https://doi.org/10.1073/pnas.0800790105
geographic Southern Ocean
geographic_facet Southern Ocean
genre Elephant Seals
Mirounga leonina
Sea ice
Southern Elephant Seals
Southern Ocean
genre_facet Elephant Seals
Mirounga leonina
Sea ice
Southern Elephant Seals
Southern Ocean
op_relation Charrassin, J.-B.; Hindell, M.; Rintoul, S.R.; Roquet, F.; Sokolov, S.; Biuw, M.; Costa, D.; Boehme, L.; Lovell, P.; Coleman, R.; Timmerman, R.; Meijers, A.; Meredith, M. orcid:0000-0002-7342-7756
Park, Y.-H.; Bailleul, F.; Goebel, M.; Tremblay, Y.; Bost, C.-A.; McMahon, C.; Field, I.C.; Fedak, M.A.; Guinet, C. 2008 Southern Ocean frontal structure and sea ice formation rates revealed by elephant seals. Proceedings of the National Academy of Sciences, 105 (33), Proceedings of the National Academy of Sciences. 11,634-11,639. https://doi.org/10.1073/pnas.0800790105 <https://doi.org/10.1073/pnas.0800790105>
op_doi https://doi.org/10.1073/pnas.0800790105
container_title Proceedings of the National Academy of Sciences
container_volume 105
container_issue 33
container_start_page 11634
op_container_end_page 11639
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