The Antarctic Peninsula Under a 1.5°C Global Warming Scenario

Warming of the Antarctic Peninsula in the latter half of the twentieth century was greater than any other terrestrial environment in the Southern Hemisphere, and clear cryospheric and biological consequences have been observed. Under a global 1.5◦C scenario, warming in the Antarctic Peninsula is lik...

Full description

Bibliographic Details
Published in:Frontiers in Environmental Science
Main Authors: Siegert, M, Atkinson, A, Banwell, A, Brandon, M, Convey, P, Davies, B, Downie, R, Edwards, T, Hubbard, B, Marshall, G, Rogelj, J, Rumble, J, Stroeve, J, Vaughan, D
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers in Environmental Science 2019
Subjects:
Online Access:http://plymsea.ac.uk/id/eprint/8888/
http://plymsea.ac.uk/id/eprint/8888/1/Siegert%20et%20al%20%282019%29%20Frontiers%20in%20Env%20Sci.pdf
https://doi.org/10.3389/fenvs.2019.00102
id ftplymouthml:oai:plymsea.ac.uk:8888
record_format openpolar
spelling ftplymouthml:oai:plymsea.ac.uk:8888 2023-05-15T13:57:48+02:00 The Antarctic Peninsula Under a 1.5°C Global Warming Scenario Siegert, M Atkinson, A Banwell, A Brandon, M Convey, P Davies, B Downie, R Edwards, T Hubbard, B Marshall, G Rogelj, J Rumble, J Stroeve, J Vaughan, D 2019-06-28 text http://plymsea.ac.uk/id/eprint/8888/ http://plymsea.ac.uk/id/eprint/8888/1/Siegert%20et%20al%20%282019%29%20Frontiers%20in%20Env%20Sci.pdf https://doi.org/10.3389/fenvs.2019.00102 en eng Frontiers in Environmental Science http://plymsea.ac.uk/id/eprint/8888/1/Siegert%20et%20al%20%282019%29%20Frontiers%20in%20Env%20Sci.pdf Siegert, M; Atkinson, A; Banwell, A; Brandon, M; Convey, P; Davies, B; Downie, R; Edwards, T; Hubbard, B; Marshall, G; Rogelj, J; Rumble, J; Stroeve, J; Vaughan, D. 2019 The Antarctic Peninsula Under a 1.5°C Global Warming Scenario. Frontiers in Environmental Science, 7. 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 ftplymouthml https://doi.org/10.3389/fenvs.2019.00102 2022-09-13T05:49:44Z Warming of the Antarctic Peninsula in the latter half of the twentieth century was greater than any other terrestrial environment in the Southern Hemisphere, and clear cryospheric and biological consequences have been observed. Under a global 1.5◦C scenario, warming in the Antarctic Peninsula is likely to 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* Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML) Antarctic The Antarctic Antarctic Peninsula Frontiers in Environmental Science 7
institution Open Polar
collection Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML)
op_collection_id ftplymouthml
language English
description Warming of the Antarctic Peninsula in the latter half of the twentieth century was greater than any other terrestrial environment in the Southern Hemisphere, and clear cryospheric and biological consequences have been observed. Under a global 1.5◦C scenario, warming in the Antarctic Peninsula is likely to 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, M
Atkinson, A
Banwell, A
Brandon, M
Convey, P
Davies, B
Downie, R
Edwards, T
Hubbard, B
Marshall, G
Rogelj, J
Rumble, J
Stroeve, J
Vaughan, D
spellingShingle Siegert, M
Atkinson, A
Banwell, A
Brandon, M
Convey, P
Davies, B
Downie, R
Edwards, T
Hubbard, B
Marshall, G
Rogelj, J
Rumble, J
Stroeve, J
Vaughan, D
The Antarctic Peninsula Under a 1.5°C Global Warming Scenario
author_facet Siegert, M
Atkinson, A
Banwell, A
Brandon, M
Convey, P
Davies, B
Downie, R
Edwards, T
Hubbard, B
Marshall, G
Rogelj, J
Rumble, J
Stroeve, J
Vaughan, D
author_sort Siegert, M
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 in Environmental Science
publishDate 2019
url http://plymsea.ac.uk/id/eprint/8888/
http://plymsea.ac.uk/id/eprint/8888/1/Siegert%20et%20al%20%282019%29%20Frontiers%20in%20Env%20Sci.pdf
https://doi.org/10.3389/fenvs.2019.00102
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 http://plymsea.ac.uk/id/eprint/8888/1/Siegert%20et%20al%20%282019%29%20Frontiers%20in%20Env%20Sci.pdf
Siegert, M; Atkinson, A; Banwell, A; Brandon, M; Convey, P; Davies, B; Downie, R; Edwards, T; Hubbard, B; Marshall, G; Rogelj, J; Rumble, J; Stroeve, J; Vaughan, D. 2019 The Antarctic Peninsula Under a 1.5°C Global Warming Scenario. Frontiers in Environmental Science, 7. 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
_version_ 1766265699004579840