The Antarctic Peninsula under a 1.5°C global warming scenario.

Warming of the Antarctic Peninsula in the latter half of the 20th century was greater than any other terrestrial environment in the Southern Hemisphere, and obvious cryospheric and biological consequences have been observed. Under a global 1.5°C scenario, warming in the Antarctic Peninsula is likely...

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Published in:Frontiers in Environmental Science
Main Authors: Siegert, Martin, Atkinson, Angus, Banwell, Alison, Brandon, Mark, Convey, Peter, Davies, Bethan, Downie, Rod, Edwards, Tamsin, Hubbard, Bryn, Marshall, Gareth, Rogelj, Joeri, Rumble, Jane, Stroeve, Julienne, Vaughan, David
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media SA 2019
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/522830/
https://nora.nerc.ac.uk/id/eprint/522830/1/fenvs-07-00102.pdf
https://www.frontiersin.org/articles/10.3389/fenvs.2019.00102/abstract
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spelling ftnerc:oai:nora.nerc.ac.uk:522830 2023-05-15T13:41:43+02:00 The Antarctic Peninsula under a 1.5°C global warming scenario. Siegert, Martin Atkinson, Angus Banwell, Alison Brandon, Mark Convey, Peter Davies, Bethan Downie, Rod Edwards, Tamsin Hubbard, Bryn Marshall, Gareth Rogelj, Joeri Rumble, Jane Stroeve, Julienne Vaughan, David 2019-06-28 text http://nora.nerc.ac.uk/id/eprint/522830/ https://nora.nerc.ac.uk/id/eprint/522830/1/fenvs-07-00102.pdf https://www.frontiersin.org/articles/10.3389/fenvs.2019.00102/abstract en eng Frontiers Media SA https://nora.nerc.ac.uk/id/eprint/522830/1/fenvs-07-00102.pdf Siegert, Martin; Atkinson, Angus; Banwell, Alison; Brandon, Mark; Convey, Peter orcid:0000-0001-8497-9903 Davies, Bethan; Downie, Rod; Edwards, Tamsin; Hubbard, Bryn; Marshall, Gareth orcid:0000-0001-8887-7314 Rogelj, Joeri; Rumble, Jane; Stroeve, Julienne; Vaughan, David orcid:0000-0002-9065-0570 . 2019 The Antarctic Peninsula under a 1.5°C global warming scenario. Frontiers in Environmental Science, 7, 102. https://doi.org/10.3389/fenvs.2019.00102 <https://doi.org/10.3389/fenvs.2019.00102> cc_by_4 CC-BY Publication - Article PeerReviewed 2019 ftnerc https://doi.org/10.3389/fenvs.2019.00102 2023-02-04T19:48:04Z Warming of the Antarctic Peninsula in the latter half of the 20th century was greater than any other terrestrial environment in the Southern Hemisphere, and obvious cryospheric and biological consequences have been observed. Under a global 1.5°C scenario, warming in the Antarctic Peninsula is likely increase the number of days above 0°C, with up to 130 of such days each year in the northern Peninsula. Ocean turbulence will increase, making the circumpolar deep water (CDW) both warmer and shallower, delivering heat to the sea surface and to coastal margins. Thinning and recession of marine margins of glaciers and ice caps is expected to accelerate to terrestrial limits, increasing iceberg production, after which glacier retreat may slow on land. Ice shelves will experience continued increase in meltwater production and consequent structural change, but not imminent regional collapses. Marine biota can respond in multiple ways to climatic changes, with effects complicated by past resource extraction activities. Southward distribution shifts have been observed in multiple taxa during the last century and these are likely to continue. Exposed (ice free) terrestrial areas will expand, providing new habitats for native and non-native organisms, but with a potential loss of genetic diversity. While native terrestrial biota are likely to benefit from modest warming, the greatest threat to native biodiversity is from non-native terrestrial species. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ice Shelves Iceberg* Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Antarctic Peninsula Frontiers in Environmental Science 7
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
description Warming of the Antarctic Peninsula in the latter half of the 20th century was greater than any other terrestrial environment in the Southern Hemisphere, and obvious cryospheric and biological consequences have been observed. Under a global 1.5°C scenario, warming in the Antarctic Peninsula is likely increase the number of days above 0°C, with up to 130 of such days each year in the northern Peninsula. Ocean turbulence will increase, making the circumpolar deep water (CDW) both warmer and shallower, delivering heat to the sea surface and to coastal margins. Thinning and recession of marine margins of glaciers and ice caps is expected to accelerate to terrestrial limits, increasing iceberg production, after which glacier retreat may slow on land. Ice shelves will experience continued increase in meltwater production and consequent structural change, but not imminent regional collapses. Marine biota can respond in multiple ways to climatic changes, with effects complicated by past resource extraction activities. Southward distribution shifts have been observed in multiple taxa during the last century and these are likely to continue. Exposed (ice free) terrestrial areas will expand, providing new habitats for native and non-native organisms, but with a potential loss of genetic diversity. While native terrestrial biota are likely to benefit from modest warming, the greatest threat to native biodiversity is from non-native terrestrial species.
format Article in Journal/Newspaper
author Siegert, Martin
Atkinson, Angus
Banwell, Alison
Brandon, Mark
Convey, Peter
Davies, Bethan
Downie, Rod
Edwards, Tamsin
Hubbard, Bryn
Marshall, Gareth
Rogelj, Joeri
Rumble, Jane
Stroeve, Julienne
Vaughan, David
spellingShingle Siegert, Martin
Atkinson, Angus
Banwell, Alison
Brandon, Mark
Convey, Peter
Davies, Bethan
Downie, Rod
Edwards, Tamsin
Hubbard, Bryn
Marshall, Gareth
Rogelj, Joeri
Rumble, Jane
Stroeve, Julienne
Vaughan, David
The Antarctic Peninsula under a 1.5°C global warming scenario.
author_facet Siegert, Martin
Atkinson, Angus
Banwell, Alison
Brandon, Mark
Convey, Peter
Davies, Bethan
Downie, Rod
Edwards, Tamsin
Hubbard, Bryn
Marshall, Gareth
Rogelj, Joeri
Rumble, Jane
Stroeve, Julienne
Vaughan, David
author_sort Siegert, Martin
title The Antarctic Peninsula under a 1.5°C global warming scenario.
title_short The Antarctic Peninsula under a 1.5°C global warming scenario.
title_full The Antarctic Peninsula under a 1.5°C global warming scenario.
title_fullStr The Antarctic Peninsula under a 1.5°C global warming scenario.
title_full_unstemmed The Antarctic Peninsula under a 1.5°C global warming scenario.
title_sort antarctic peninsula under a 1.5°c global warming scenario.
publisher Frontiers Media SA
publishDate 2019
url http://nora.nerc.ac.uk/id/eprint/522830/
https://nora.nerc.ac.uk/id/eprint/522830/1/fenvs-07-00102.pdf
https://www.frontiersin.org/articles/10.3389/fenvs.2019.00102/abstract
geographic Antarctic
The Antarctic
Antarctic Peninsula
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
genre Antarc*
Antarctic
Antarctic Peninsula
Ice Shelves
Iceberg*
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Ice Shelves
Iceberg*
op_relation https://nora.nerc.ac.uk/id/eprint/522830/1/fenvs-07-00102.pdf
Siegert, Martin; Atkinson, Angus; Banwell, Alison; Brandon, Mark; Convey, Peter orcid:0000-0001-8497-9903
Davies, Bethan; Downie, Rod; Edwards, Tamsin; Hubbard, Bryn; Marshall, Gareth orcid:0000-0001-8887-7314
Rogelj, Joeri; Rumble, Jane; Stroeve, Julienne; Vaughan, David orcid:0000-0002-9065-0570 . 2019 The Antarctic Peninsula under a 1.5°C global warming scenario. Frontiers in Environmental Science, 7, 102. https://doi.org/10.3389/fenvs.2019.00102 <https://doi.org/10.3389/fenvs.2019.00102>
op_rights cc_by_4
op_rightsnorm CC-BY
op_doi https://doi.org/10.3389/fenvs.2019.00102
container_title Frontiers in Environmental Science
container_volume 7
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