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, Moore, John C.
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://research.ulapland.fi/fi/publications/bbb28a0a-86d1-425b-92ec-c601286ac730
https://doi.org/10.5194/tc-12-2955-2018
http://www.scopus.com/inward/record.url?scp=85053905908&partnerID=8YFLogxK
http://www.scopus.com/inward/citedby.url?scp=85053905908&partnerID=8YFLogxK
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spelling ftulaplandcdispu:oai:lacris.ulapland.fi:publications/bbb28a0a-86d1-425b-92ec-c601286ac730 2024-06-23T07:47:21+00:00 Stopping the flood:could we use targeted geoengineering to mitigate sea level rise? Wolovick, Michael Moore, John C. 2018-09-20 https://research.ulapland.fi/fi/publications/bbb28a0a-86d1-425b-92ec-c601286ac730 https://doi.org/10.5194/tc-12-2955-2018 http://www.scopus.com/inward/record.url?scp=85053905908&partnerID=8YFLogxK http://www.scopus.com/inward/citedby.url?scp=85053905908&partnerID=8YFLogxK eng eng https://research.ulapland.fi/fi/publications/bbb28a0a-86d1-425b-92ec-c601286ac730 info:eu-repo/semantics/openAccess Wolovick , M & Moore , J C 2018 , ' Stopping the flood : could we use targeted geoengineering to mitigate sea level rise? ' , Cryosphere , vol. 12 , no. 9 , pp. 2955-2967 . https://doi.org/10.5194/tc-12-2955-2018 /dk/atira/pure/person/fieldofscience2010/1/17/1 name=Geosciences article 2018 ftulaplandcdispu https://doi.org/10.5194/tc-12-2955-2018 2024-05-27T23:39:57Z 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 Thwaites Glacier West Antarctica LaCRIS - University of Lapland Current Research System 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 LaCRIS - University of Lapland Current Research System
op_collection_id ftulaplandcdispu
language English
topic /dk/atira/pure/person/fieldofscience2010/1/17/1
name=Geosciences
spellingShingle /dk/atira/pure/person/fieldofscience2010/1/17/1
name=Geosciences
Wolovick, Michael
Moore, John C.
Stopping the flood:could we use targeted geoengineering to mitigate sea level rise?
topic_facet /dk/atira/pure/person/fieldofscience2010/1/17/1
name=Geosciences
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
Moore, John C.
author_facet Wolovick, Michael
Moore, John C.
author_sort Wolovick, Michael
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?
publishDate 2018
url https://research.ulapland.fi/fi/publications/bbb28a0a-86d1-425b-92ec-c601286ac730
https://doi.org/10.5194/tc-12-2955-2018
http://www.scopus.com/inward/record.url?scp=85053905908&partnerID=8YFLogxK
http://www.scopus.com/inward/citedby.url?scp=85053905908&partnerID=8YFLogxK
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
Thwaites Glacier
West Antarctica
genre_facet Antarc*
Antarctica
Ice Sheet
Ice Shelf
Thwaites Glacier
West Antarctica
op_source Wolovick , M & Moore , J C 2018 , ' Stopping the flood : could we use targeted geoengineering to mitigate sea level rise? ' , Cryosphere , vol. 12 , no. 9 , pp. 2955-2967 . https://doi.org/10.5194/tc-12-2955-2018
op_relation https://research.ulapland.fi/fi/publications/bbb28a0a-86d1-425b-92ec-c601286ac730
op_rights info:eu-repo/semantics/openAccess
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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