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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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 |
_version_ |
1801375176964702208 |