Increasing Arctic Sea Ice Albedo Using Localized Reversible Geoengineering

Abstract The rising costs of climate change merit serious evaluation of potential climate restoration solutions. The highest rate of change in climate is observed in the Arctic where the summer ice is diminishing at an accelerated rate. The loss of Arctic sea ice increases radiative forcing and cont...

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Published in:Earth's Future
Main Authors: L. Field, D. Ivanova, S. Bhattacharyya, V. Mlaker, A. Sholtz, R. Decca, A. Manzara, D. Johnson, E. Christodoulou, P. Walter, K. Katuri
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2018
Subjects:
Online Access:https://doi.org/10.1029/2018EF000820
https://doaj.org/article/dd868d416cb24bf78cc42618d5259f66
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spelling ftdoajarticles:oai:doaj.org/article:dd868d416cb24bf78cc42618d5259f66 2023-05-15T13:10:26+02:00 Increasing Arctic Sea Ice Albedo Using Localized Reversible Geoengineering L. Field D. Ivanova S. Bhattacharyya V. Mlaker A. Sholtz R. Decca A. Manzara D. Johnson E. Christodoulou P. Walter K. Katuri 2018-06-01T00:00:00Z https://doi.org/10.1029/2018EF000820 https://doaj.org/article/dd868d416cb24bf78cc42618d5259f66 EN eng Wiley https://doi.org/10.1029/2018EF000820 https://doaj.org/toc/2328-4277 2328-4277 doi:10.1029/2018EF000820 https://doaj.org/article/dd868d416cb24bf78cc42618d5259f66 Earth's Future, Vol 6, Iss 6, Pp 882-901 (2018) Arctic ice restoration geoengineering albedo modification 2018 IPCC 1.5° climate change climate modeling Environmental sciences GE1-350 Ecology QH540-549.5 article 2018 ftdoajarticles https://doi.org/10.1029/2018EF000820 2022-12-31T01:02:54Z Abstract The rising costs of climate change merit serious evaluation of potential climate restoration solutions. The highest rate of change in climate is observed in the Arctic where the summer ice is diminishing at an accelerated rate. The loss of Arctic sea ice increases radiative forcing and contributes to global warming. Restoring reflectivity of Arctic ice could be a powerful lever to help in the effort to limit global warming to 1.5°C. Polar ice restoration should be considered in planning of 1.5°C pathways. In this paper, a novel localized surface albedo modification technique is presented that shows promise as a method to increase multiyear ice using reflective floating materials, chosen so as to have low subsidiary environmental impact. Detailed climate modeling studying the climate impact of such a method reveals more than 1.5°C cooler temperatures over a large part of the Arctic when simulating global sea ice albedo modification. In a region north of Barents and Kara Seas temperatures have been reduced by 3°C and in North Canada by almost 1°C. Additionally, there are notable increases in sea ice thickness (20–50 cm Arctic wide) and ice concentration (>15–20% across large parts of central Arctic). These results suggest that the geoengineering technology proposed in this study may be a viable instrument for restoring Arctic ice. Article in Journal/Newspaper albedo Arctic Central Arctic Climate change Global warming Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Canada Lever ENVELOPE(-63.608,-63.608,-65.506,-65.506) Earth's Future 6 6 882 901
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic ice restoration
geoengineering
albedo modification
2018 IPCC 1.5°
climate change
climate modeling
Environmental sciences
GE1-350
Ecology
QH540-549.5
spellingShingle Arctic ice restoration
geoengineering
albedo modification
2018 IPCC 1.5°
climate change
climate modeling
Environmental sciences
GE1-350
Ecology
QH540-549.5
L. Field
D. Ivanova
S. Bhattacharyya
V. Mlaker
A. Sholtz
R. Decca
A. Manzara
D. Johnson
E. Christodoulou
P. Walter
K. Katuri
Increasing Arctic Sea Ice Albedo Using Localized Reversible Geoengineering
topic_facet Arctic ice restoration
geoengineering
albedo modification
2018 IPCC 1.5°
climate change
climate modeling
Environmental sciences
GE1-350
Ecology
QH540-549.5
description Abstract The rising costs of climate change merit serious evaluation of potential climate restoration solutions. The highest rate of change in climate is observed in the Arctic where the summer ice is diminishing at an accelerated rate. The loss of Arctic sea ice increases radiative forcing and contributes to global warming. Restoring reflectivity of Arctic ice could be a powerful lever to help in the effort to limit global warming to 1.5°C. Polar ice restoration should be considered in planning of 1.5°C pathways. In this paper, a novel localized surface albedo modification technique is presented that shows promise as a method to increase multiyear ice using reflective floating materials, chosen so as to have low subsidiary environmental impact. Detailed climate modeling studying the climate impact of such a method reveals more than 1.5°C cooler temperatures over a large part of the Arctic when simulating global sea ice albedo modification. In a region north of Barents and Kara Seas temperatures have been reduced by 3°C and in North Canada by almost 1°C. Additionally, there are notable increases in sea ice thickness (20–50 cm Arctic wide) and ice concentration (>15–20% across large parts of central Arctic). These results suggest that the geoengineering technology proposed in this study may be a viable instrument for restoring Arctic ice.
format Article in Journal/Newspaper
author L. Field
D. Ivanova
S. Bhattacharyya
V. Mlaker
A. Sholtz
R. Decca
A. Manzara
D. Johnson
E. Christodoulou
P. Walter
K. Katuri
author_facet L. Field
D. Ivanova
S. Bhattacharyya
V. Mlaker
A. Sholtz
R. Decca
A. Manzara
D. Johnson
E. Christodoulou
P. Walter
K. Katuri
author_sort L. Field
title Increasing Arctic Sea Ice Albedo Using Localized Reversible Geoengineering
title_short Increasing Arctic Sea Ice Albedo Using Localized Reversible Geoengineering
title_full Increasing Arctic Sea Ice Albedo Using Localized Reversible Geoengineering
title_fullStr Increasing Arctic Sea Ice Albedo Using Localized Reversible Geoengineering
title_full_unstemmed Increasing Arctic Sea Ice Albedo Using Localized Reversible Geoengineering
title_sort increasing arctic sea ice albedo using localized reversible geoengineering
publisher Wiley
publishDate 2018
url https://doi.org/10.1029/2018EF000820
https://doaj.org/article/dd868d416cb24bf78cc42618d5259f66
long_lat ENVELOPE(-63.608,-63.608,-65.506,-65.506)
geographic Arctic
Canada
Lever
geographic_facet Arctic
Canada
Lever
genre albedo
Arctic
Central Arctic
Climate change
Global warming
Sea ice
genre_facet albedo
Arctic
Central Arctic
Climate change
Global warming
Sea ice
op_source Earth's Future, Vol 6, Iss 6, Pp 882-901 (2018)
op_relation https://doi.org/10.1029/2018EF000820
https://doaj.org/toc/2328-4277
2328-4277
doi:10.1029/2018EF000820
https://doaj.org/article/dd868d416cb24bf78cc42618d5259f66
op_doi https://doi.org/10.1029/2018EF000820
container_title Earth's Future
container_volume 6
container_issue 6
container_start_page 882
op_container_end_page 901
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