Subglacial discharge plume behaviour revealed by CTD-instrumented ringed seals

Subglacial discharge plumes increase submarine melting of marine-terminating glaciers significantly; however, in-situ data on their properties and behaviour are limited. We present oceanographic data collected by ringed seals (Pusa hispida) instrumented with GPS-equipped conductivity-temperature-dep...

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Published in:Scientific Reports
Main Authors: Everett, Alistair, Kohler, Jack, Sundfjord, Arild, Kovacs, Kit M., Torsvik, Tomas, Pramanik, Ankit, Boehme, Lars, Lydersen, Christian
Format: Text
Language:English
Published: Nature Publishing Group UK 2018
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6128829/
http://www.ncbi.nlm.nih.gov/pubmed/30194352
https://doi.org/10.1038/s41598-018-31875-8
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author Everett, Alistair
Kohler, Jack
Sundfjord, Arild
Kovacs, Kit M.
Torsvik, Tomas
Pramanik, Ankit
Boehme, Lars
Lydersen, Christian
author_facet Everett, Alistair
Kohler, Jack
Sundfjord, Arild
Kovacs, Kit M.
Torsvik, Tomas
Pramanik, Ankit
Boehme, Lars
Lydersen, Christian
author_sort Everett, Alistair
collection PubMed Central (PMC)
container_issue 1
container_title Scientific Reports
container_volume 8
description Subglacial discharge plumes increase submarine melting of marine-terminating glaciers significantly; however, in-situ data on their properties and behaviour are limited. We present oceanographic data collected by ringed seals (Pusa hispida) instrumented with GPS-equipped conductivity-temperature-depth satellite relay data loggers (GPS-CTD-SRDLs) in Kongsfjorden, Svalbard, during 2012. The seals foraged just outside the plumes and collected hydrographic data from within the plumes’ upwelling cores as they returned to the surface. The seals encountered water with fractions of subglacial discharge as high as 27% at 60 m below the ocean surface. The ringed seals responded rapidly to spatial and temporal variations in subglacial discharge at the glacier terminus, suggesting that prey becomes available quickly following the appearance of plumes. The seals’ dive locations were used to monitor the presence of plumes over a four-month period. High surface runoff from Kronebreen catchment created strong plumes, but weak plumes were present even during periods of low surface runoff. The continued retreat of Kronebreen, and other tidewater glaciers, will lead to the loss of these marine-termini as the glaciers retreat onto land. The techniques presented here improve our understanding of the drivers of glacial retreat and the implications of future habitat loss for glacier-associated birds and mammals.
format Text
genre glacier
Kongsfjord*
Kongsfjorden
Pusa hispida
Svalbard
Tidewater
genre_facet glacier
Kongsfjord*
Kongsfjorden
Pusa hispida
Svalbard
Tidewater
geographic Svalbard
Kronebreen
geographic_facet Svalbard
Kronebreen
id ftpubmed:oai:pubmedcentral.nih.gov:6128829
institution Open Polar
language English
long_lat ENVELOPE(13.333,13.333,78.833,78.833)
op_collection_id ftpubmed
op_doi https://doi.org/10.1038/s41598-018-31875-8
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6128829/
http://www.ncbi.nlm.nih.gov/pubmed/30194352
http://dx.doi.org/10.1038/s41598-018-31875-8
op_rights © The Author(s) 2018
Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
op_rightsnorm CC-BY
publishDate 2018
publisher Nature Publishing Group UK
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spelling ftpubmed:oai:pubmedcentral.nih.gov:6128829 2025-01-16T22:03:27+00:00 Subglacial discharge plume behaviour revealed by CTD-instrumented ringed seals Everett, Alistair Kohler, Jack Sundfjord, Arild Kovacs, Kit M. Torsvik, Tomas Pramanik, Ankit Boehme, Lars Lydersen, Christian 2018-09-07 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6128829/ http://www.ncbi.nlm.nih.gov/pubmed/30194352 https://doi.org/10.1038/s41598-018-31875-8 en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6128829/ http://www.ncbi.nlm.nih.gov/pubmed/30194352 http://dx.doi.org/10.1038/s41598-018-31875-8 © The Author(s) 2018 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. CC-BY Article Text 2018 ftpubmed https://doi.org/10.1038/s41598-018-31875-8 2018-09-16T00:21:12Z Subglacial discharge plumes increase submarine melting of marine-terminating glaciers significantly; however, in-situ data on their properties and behaviour are limited. We present oceanographic data collected by ringed seals (Pusa hispida) instrumented with GPS-equipped conductivity-temperature-depth satellite relay data loggers (GPS-CTD-SRDLs) in Kongsfjorden, Svalbard, during 2012. The seals foraged just outside the plumes and collected hydrographic data from within the plumes’ upwelling cores as they returned to the surface. The seals encountered water with fractions of subglacial discharge as high as 27% at 60 m below the ocean surface. The ringed seals responded rapidly to spatial and temporal variations in subglacial discharge at the glacier terminus, suggesting that prey becomes available quickly following the appearance of plumes. The seals’ dive locations were used to monitor the presence of plumes over a four-month period. High surface runoff from Kronebreen catchment created strong plumes, but weak plumes were present even during periods of low surface runoff. The continued retreat of Kronebreen, and other tidewater glaciers, will lead to the loss of these marine-termini as the glaciers retreat onto land. The techniques presented here improve our understanding of the drivers of glacial retreat and the implications of future habitat loss for glacier-associated birds and mammals. Text glacier Kongsfjord* Kongsfjorden Pusa hispida Svalbard Tidewater PubMed Central (PMC) Svalbard Kronebreen ENVELOPE(13.333,13.333,78.833,78.833) Scientific Reports 8 1
spellingShingle Article
Everett, Alistair
Kohler, Jack
Sundfjord, Arild
Kovacs, Kit M.
Torsvik, Tomas
Pramanik, Ankit
Boehme, Lars
Lydersen, Christian
Subglacial discharge plume behaviour revealed by CTD-instrumented ringed seals
title Subglacial discharge plume behaviour revealed by CTD-instrumented ringed seals
title_full Subglacial discharge plume behaviour revealed by CTD-instrumented ringed seals
title_fullStr Subglacial discharge plume behaviour revealed by CTD-instrumented ringed seals
title_full_unstemmed Subglacial discharge plume behaviour revealed by CTD-instrumented ringed seals
title_short Subglacial discharge plume behaviour revealed by CTD-instrumented ringed seals
title_sort subglacial discharge plume behaviour revealed by ctd-instrumented ringed seals
topic Article
topic_facet Article
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6128829/
http://www.ncbi.nlm.nih.gov/pubmed/30194352
https://doi.org/10.1038/s41598-018-31875-8