Stopping the flood: could we use targeted geoengineering to mitigate sea level rise?

The Marine Ice Sheet Instability (MISI) is a dynamic feedback that can cause an ice sheet to enter a runaway collapse. Thwaites Glacier, West Antarctica, is projected to be the largest individual source of future sea level rise and may have already entered MISI. Here, we use a suite of coupled quasi...

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Published in:The Cryosphere
Main Authors: Wolovick, Michael J., Moore, John C.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-12-2955-2018
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00004626 2023-05-15T13:34:49+02:00 Stopping the flood: could we use targeted geoengineering to mitigate sea level rise? Wolovick, Michael J. Moore, John C. 2018-09 electronic https://doi.org/10.5194/tc-12-2955-2018 https://noa.gwlb.de/receive/cop_mods_00004626 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00004583/tc-12-2955-2018.pdf https://tc.copernicus.org/articles/12/2955/2018/tc-12-2955-2018.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-12-2955-2018 https://noa.gwlb.de/receive/cop_mods_00004626 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00004583/tc-12-2955-2018.pdf https://tc.copernicus.org/articles/12/2955/2018/tc-12-2955-2018.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2018 ftnonlinearchiv https://doi.org/10.5194/tc-12-2955-2018 2022-02-08T22:59:59Z The Marine Ice Sheet Instability (MISI) is a dynamic feedback that can cause an ice sheet to enter a runaway collapse. Thwaites Glacier, West Antarctica, is projected to be the largest individual source of future sea level rise and may have already entered MISI. Here, we use a suite of coupled quasi-2-D ice–ocean simulations to explore whether targeted geoengineering using either a continuous artificial sill or isolated artificial pinning points could counter a collapse. Successful interventions occur when the floating ice shelf regrounds on the structure, increasing buttressing and reducing ice flux across the grounding line. Regrounding is more likely with a continuous sill that is able to block warm water transport to the grounding line. The smallest design we consider is comparable in scale to existing civil engineering projects but only has a 30 % success rate, while larger designs are more effective. There are multiple possible routes forward to improve upon the designs that we considered, and with decades or more to research designs it is plausible that the scientific community could come up with a plan that is both effective and achievable. While reducing emissions remains the short-term priority for minimizing the effects of climate change, in the long run humanity may need to develop contingency plans to deal with an ice sheet collapse. Article in Journal/Newspaper Antarc* Antarctica Ice Sheet Ice Shelf The Cryosphere Thwaites Glacier West Antarctica Niedersächsisches Online-Archiv NOA Misi ENVELOPE(26.683,26.683,66.617,66.617) Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500) West Antarctica The Cryosphere 12 9 2955 2967
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Wolovick, Michael J.
Moore, John C.
Stopping the flood: could we use targeted geoengineering to mitigate sea level rise?
topic_facet article
Verlagsveröffentlichung
description The Marine Ice Sheet Instability (MISI) is a dynamic feedback that can cause an ice sheet to enter a runaway collapse. Thwaites Glacier, West Antarctica, is projected to be the largest individual source of future sea level rise and may have already entered MISI. Here, we use a suite of coupled quasi-2-D ice–ocean simulations to explore whether targeted geoengineering using either a continuous artificial sill or isolated artificial pinning points could counter a collapse. Successful interventions occur when the floating ice shelf regrounds on the structure, increasing buttressing and reducing ice flux across the grounding line. Regrounding is more likely with a continuous sill that is able to block warm water transport to the grounding line. The smallest design we consider is comparable in scale to existing civil engineering projects but only has a 30 % success rate, while larger designs are more effective. There are multiple possible routes forward to improve upon the designs that we considered, and with decades or more to research designs it is plausible that the scientific community could come up with a plan that is both effective and achievable. While reducing emissions remains the short-term priority for minimizing the effects of climate change, in the long run humanity may need to develop contingency plans to deal with an ice sheet collapse.
format Article in Journal/Newspaper
author Wolovick, Michael J.
Moore, John C.
author_facet Wolovick, Michael J.
Moore, John C.
author_sort Wolovick, Michael J.
title Stopping the flood: could we use targeted geoengineering to mitigate sea level rise?
title_short Stopping the flood: could we use targeted geoengineering to mitigate sea level rise?
title_full Stopping the flood: could we use targeted geoengineering to mitigate sea level rise?
title_fullStr Stopping the flood: could we use targeted geoengineering to mitigate sea level rise?
title_full_unstemmed Stopping the flood: could we use targeted geoengineering to mitigate sea level rise?
title_sort stopping the flood: could we use targeted geoengineering to mitigate sea level rise?
publisher Copernicus Publications
publishDate 2018
url https://doi.org/10.5194/tc-12-2955-2018
https://noa.gwlb.de/receive/cop_mods_00004626
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00004583/tc-12-2955-2018.pdf
https://tc.copernicus.org/articles/12/2955/2018/tc-12-2955-2018.pdf
long_lat ENVELOPE(26.683,26.683,66.617,66.617)
ENVELOPE(-106.750,-106.750,-75.500,-75.500)
geographic Misi
Thwaites Glacier
West Antarctica
geographic_facet Misi
Thwaites Glacier
West Antarctica
genre Antarc*
Antarctica
Ice Sheet
Ice Shelf
The Cryosphere
Thwaites Glacier
West Antarctica
genre_facet Antarc*
Antarctica
Ice Sheet
Ice Shelf
The Cryosphere
Thwaites Glacier
West Antarctica
op_relation The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424
https://doi.org/10.5194/tc-12-2955-2018
https://noa.gwlb.de/receive/cop_mods_00004626
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00004583/tc-12-2955-2018.pdf
https://tc.copernicus.org/articles/12/2955/2018/tc-12-2955-2018.pdf
op_rights https://creativecommons.org/licenses/by/4.0/
uneingeschränkt
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5194/tc-12-2955-2018
container_title The Cryosphere
container_volume 12
container_issue 9
container_start_page 2955
op_container_end_page 2967
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