The Antarctic Ice Sheet's response to idealised geoengineering scenarios ...

<!--!introduction!--> Sea level will continue to rise beyond the 22 nd century due to inertia in the climate system, even if temperatures were immediately stabilised, leading to the proposal of more dramatic measures, such as geoengineering. To provide initial sea level contribution (SLC) esti...

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Main Authors: Adhikari, Mira, Martin, Daniel F., Edwards, Tamsin, Payne, Antony J., O'Neill, James
Format: Conference Object
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-2914
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018967
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spelling ftdatacite:10.57757/iugg23-2914 2023-07-23T04:15:43+02:00 The Antarctic Ice Sheet's response to idealised geoengineering scenarios ... Adhikari, Mira Martin, Daniel F. Edwards, Tamsin Payne, Antony J. O'Neill, James 2023 https://dx.doi.org/10.57757/iugg23-2914 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018967 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Article ConferencePaper Oral 2023 ftdatacite https://doi.org/10.57757/iugg23-2914 2023-07-03T18:42:54Z <!--!introduction!--> Sea level will continue to rise beyond the 22 nd century due to inertia in the climate system, even if temperatures were immediately stabilised, leading to the proposal of more dramatic measures, such as geoengineering. To provide initial sea level contribution (SLC) estimates from the AIS and address long-term commitment and reversibility questions, a set of idealized geoengineering scenarios were performed with the BISICLES ice sheet model. Climate forcings were extended beyond 2100 to 2200 by either fixing the climate at 2100 (2050) levels at the end (middle) of the century (commitment scenarios), or immediately returning to 2015 levels (e.g. via an instantaneous implementation of geoengineering). Results show that for both high (RCP8.5) and low (RCP2.6) forcing scenarios, reverting back to 2015 climate does not prevent significant loss from the AIS. However, if geoengineering methods are adopted in 2050, SLC is lower than in the commitment scenarios. If geoengineering is ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Conference Object Antarc* Antarctic Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Antarctic The Antarctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
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description <!--!introduction!--> Sea level will continue to rise beyond the 22 nd century due to inertia in the climate system, even if temperatures were immediately stabilised, leading to the proposal of more dramatic measures, such as geoengineering. To provide initial sea level contribution (SLC) estimates from the AIS and address long-term commitment and reversibility questions, a set of idealized geoengineering scenarios were performed with the BISICLES ice sheet model. Climate forcings were extended beyond 2100 to 2200 by either fixing the climate at 2100 (2050) levels at the end (middle) of the century (commitment scenarios), or immediately returning to 2015 levels (e.g. via an instantaneous implementation of geoengineering). Results show that for both high (RCP8.5) and low (RCP2.6) forcing scenarios, reverting back to 2015 climate does not prevent significant loss from the AIS. However, if geoengineering methods are adopted in 2050, SLC is lower than in the commitment scenarios. If geoengineering is ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...
format Conference Object
author Adhikari, Mira
Martin, Daniel F.
Edwards, Tamsin
Payne, Antony J.
O'Neill, James
spellingShingle Adhikari, Mira
Martin, Daniel F.
Edwards, Tamsin
Payne, Antony J.
O'Neill, James
The Antarctic Ice Sheet's response to idealised geoengineering scenarios ...
author_facet Adhikari, Mira
Martin, Daniel F.
Edwards, Tamsin
Payne, Antony J.
O'Neill, James
author_sort Adhikari, Mira
title The Antarctic Ice Sheet's response to idealised geoengineering scenarios ...
title_short The Antarctic Ice Sheet's response to idealised geoengineering scenarios ...
title_full The Antarctic Ice Sheet's response to idealised geoengineering scenarios ...
title_fullStr The Antarctic Ice Sheet's response to idealised geoengineering scenarios ...
title_full_unstemmed The Antarctic Ice Sheet's response to idealised geoengineering scenarios ...
title_sort antarctic ice sheet's response to idealised geoengineering scenarios ...
publisher GFZ German Research Centre for Geosciences
publishDate 2023
url https://dx.doi.org/10.57757/iugg23-2914
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018967
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
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Antarctic
Ice Sheet
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.57757/iugg23-2914
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