A high-end sea level rise probabilistic projection including rapid Antarctic ice sheet mass loss

The potential for break-up of Antarctic ice shelves by hydrofracturing and following ice cliff instability might be important for future ice dynamics. One recent study suggests that the Antarctic ice sheet could lose a lot more mass during the 21st century than previously thought. This increased mas...

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Published in:Environmental Research Letters
Main Authors: Dewi Le Bars, Sybren Drijfhout, Hylke de Vries
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2017
Subjects:
Q
Online Access:https://doi.org/10.1088/1748-9326/aa6512
https://doaj.org/article/869d7e4014774464b22479e726d18329
id ftdoajarticles:oai:doaj.org/article:869d7e4014774464b22479e726d18329
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spelling ftdoajarticles:oai:doaj.org/article:869d7e4014774464b22479e726d18329 2023-09-05T13:12:28+02:00 A high-end sea level rise probabilistic projection including rapid Antarctic ice sheet mass loss Dewi Le Bars Sybren Drijfhout Hylke de Vries 2017-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/aa6512 https://doaj.org/article/869d7e4014774464b22479e726d18329 EN eng IOP Publishing https://doi.org/10.1088/1748-9326/aa6512 https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/aa6512 1748-9326 https://doaj.org/article/869d7e4014774464b22479e726d18329 Environmental Research Letters, Vol 12, Iss 4, p 044013 (2017) sea level rise antarctica probabilistic projections extreme pathways high-end projections Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2017 ftdoajarticles https://doi.org/10.1088/1748-9326/aa6512 2023-08-13T00:37:37Z The potential for break-up of Antarctic ice shelves by hydrofracturing and following ice cliff instability might be important for future ice dynamics. One recent study suggests that the Antarctic ice sheet could lose a lot more mass during the 21st century than previously thought. This increased mass-loss is found to strongly depend on the emission scenario and thereby on global temperature change. We investigate the impact of this new information on high-end global sea level rise projections by developing a probabilistic process-based method. It is shown that uncertainties in the projections increase when including the temperature dependence of Antarctic mass loss and the uncertainty in the Coupled Model Intercomparison Project Phase 5 (CMIP5) model ensemble. Including these new uncertainties we provide probability density functions for the high-end distribution of total global mean sea level in 2100 conditional on emission scenario. These projections provide a probabilistic context to previous extreme sea level scenarios developed for adaptation purposes. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Ice Shelves Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Environmental Research Letters 12 4 044013
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic sea level rise
antarctica
probabilistic projections
extreme pathways
high-end projections
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
spellingShingle sea level rise
antarctica
probabilistic projections
extreme pathways
high-end projections
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
Dewi Le Bars
Sybren Drijfhout
Hylke de Vries
A high-end sea level rise probabilistic projection including rapid Antarctic ice sheet mass loss
topic_facet sea level rise
antarctica
probabilistic projections
extreme pathways
high-end projections
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
description The potential for break-up of Antarctic ice shelves by hydrofracturing and following ice cliff instability might be important for future ice dynamics. One recent study suggests that the Antarctic ice sheet could lose a lot more mass during the 21st century than previously thought. This increased mass-loss is found to strongly depend on the emission scenario and thereby on global temperature change. We investigate the impact of this new information on high-end global sea level rise projections by developing a probabilistic process-based method. It is shown that uncertainties in the projections increase when including the temperature dependence of Antarctic mass loss and the uncertainty in the Coupled Model Intercomparison Project Phase 5 (CMIP5) model ensemble. Including these new uncertainties we provide probability density functions for the high-end distribution of total global mean sea level in 2100 conditional on emission scenario. These projections provide a probabilistic context to previous extreme sea level scenarios developed for adaptation purposes.
format Article in Journal/Newspaper
author Dewi Le Bars
Sybren Drijfhout
Hylke de Vries
author_facet Dewi Le Bars
Sybren Drijfhout
Hylke de Vries
author_sort Dewi Le Bars
title A high-end sea level rise probabilistic projection including rapid Antarctic ice sheet mass loss
title_short A high-end sea level rise probabilistic projection including rapid Antarctic ice sheet mass loss
title_full A high-end sea level rise probabilistic projection including rapid Antarctic ice sheet mass loss
title_fullStr A high-end sea level rise probabilistic projection including rapid Antarctic ice sheet mass loss
title_full_unstemmed A high-end sea level rise probabilistic projection including rapid Antarctic ice sheet mass loss
title_sort high-end sea level rise probabilistic projection including rapid antarctic ice sheet mass loss
publisher IOP Publishing
publishDate 2017
url https://doi.org/10.1088/1748-9326/aa6512
https://doaj.org/article/869d7e4014774464b22479e726d18329
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelves
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelves
op_source Environmental Research Letters, Vol 12, Iss 4, p 044013 (2017)
op_relation https://doi.org/10.1088/1748-9326/aa6512
https://doaj.org/toc/1748-9326
doi:10.1088/1748-9326/aa6512
1748-9326
https://doaj.org/article/869d7e4014774464b22479e726d18329
op_doi https://doi.org/10.1088/1748-9326/aa6512
container_title Environmental Research Letters
container_volume 12
container_issue 4
container_start_page 044013
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