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...

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Main Authors: Martin Siegert, Angus Atkinson, Alison Banwell, Mark Brandon, Peter Convey, Bethan Davies, Rod Downie, Tamsin Edwards, Bryn Hubbard, Gareth Marshall, Joeri Rogelj, Jane Rumble, Julienne Stroeve, David Vaughan
Format: Article
Language:English
Published: Frontiers Media S.A. 2019-06-01
Series:Frontiers in Environmental Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fenvs.2019.00102/full
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spelling doaj-2b7a4f45247844b78f054d73cd88ee1b2020-11-24T20:57:58ZengFrontiers Media S.A.Frontiers in Environmental Science2296-665X2019-06-01710.3389/fenvs.2019.00102465700The Antarctic Peninsula Under a 1.5°C Global Warming ScenarioMartin Siegert0Angus Atkinson1Alison Banwell2Mark Brandon3Peter Convey4Bethan Davies5Rod Downie6Tamsin Edwards7Bryn Hubbard8Gareth Marshall9Joeri Rogelj10Jane Rumble11Julienne Stroeve12Julienne Stroeve13David Vaughan14Department of Earth Science and Engineering, Grantham Institute, Imperial College London, London, United KingdomPlymouth Marine Laboratory, Plymouth, United KingdomCooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, United StatesSchool of Environment, Earth and Ecosystem Sciences, Open University, Milton Keynes, United KingdomBritish Antarctic Survey, Natural Environment Research Council (NERC), Cambridge, United KingdomCentre for Quaternary Research, Department of Geography, Royal Holloway University of London, Egham, United KingdomWWF UK, The Living Planet Centre, Woking, United KingdomDepartment of Geography, King's College London, London, United KingdomDepartment of Geography & Earth Sciences, Aberystwyth University, Aberystwyth, United KingdomBritish Antarctic Survey, Natural Environment Research Council (NERC), Cambridge, United KingdomDepartment of Earth Science and Engineering, Grantham Institute, Imperial College London, London, United Kingdom0Polar Regions Department, UK Foreign & Commonwealth Office, London, United Kingdom1Centre for Earth Observation Science, University of Manitoba, Winnipeg, Canada2Centre for Polar Observation and Modelling, University College London, London, United KingdomBritish Antarctic Survey, Natural Environment Research Council (NERC), Cambridge, United KingdomWarming 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.https://www.frontiersin.org/article/10.3389/fenvs.2019.00102/fullpolar changeglaciers and climatesea icemarine biologyterrestrial biology
collection DOAJ
language English
format Article
sources DOAJ
author Martin Siegert
Angus Atkinson
Alison Banwell
Mark Brandon
Peter Convey
Bethan Davies
Rod Downie
Tamsin Edwards
Bryn Hubbard
Gareth Marshall
Joeri Rogelj
Jane Rumble
Julienne Stroeve
Julienne Stroeve
David Vaughan
spellingShingle Martin Siegert
Angus Atkinson
Alison Banwell
Mark Brandon
Peter Convey
Bethan Davies
Rod Downie
Tamsin Edwards
Bryn Hubbard
Gareth Marshall
Joeri Rogelj
Jane Rumble
Julienne Stroeve
Julienne Stroeve
David Vaughan
The Antarctic Peninsula Under a 1.5°C Global Warming Scenario
Frontiers in Environmental Science
polar change
glaciers and climate
sea ice
marine biology
terrestrial biology
author_facet Martin Siegert
Angus Atkinson
Alison Banwell
Mark Brandon
Peter Convey
Bethan Davies
Rod Downie
Tamsin Edwards
Bryn Hubbard
Gareth Marshall
Joeri Rogelj
Jane Rumble
Julienne Stroeve
Julienne Stroeve
David Vaughan
author_sort Martin Siegert
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 S.A.
series Frontiers in Environmental Science
issn 2296-665X
publishDate 2019-06-01
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.
topic polar change
glaciers and climate
sea ice
marine biology
terrestrial biology
url https://www.frontiersin.org/article/10.3389/fenvs.2019.00102/full
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