Enhanced simulated early 21st century Arctic sea ice loss due to CMIP6 biomass burning emissions

The mechanisms underlying decadal variability in Arctic sea ice remain actively debated. Here, we ability in boreal biomass burning (BB) emissions strongly influences simulated Arctic sea ice on multidecadal time scales. In particular, we find that a strong acceleration in sea ice decline in the ear...

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Published in:Science Advances
Other Authors: DeRepentigny, Patricia (author), Jahn, Alexandra (author), Holland, Marika M. (author), Kay, Jennifer E. (author), Fasullo, John (author), Lamarque, Jean-François (author), Tilmes, Simone (author), Hannay, Cécile (author), Mills, Michael J. (author), Bailey, David A. (author), Barrett, Andrew P. (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.1126/sciadv.abo2405
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spelling ftncar:oai:drupal-site.org:articles_25613 2024-04-14T08:06:19+00:00 Enhanced simulated early 21st century Arctic sea ice loss due to CMIP6 biomass burning emissions DeRepentigny, Patricia (author) Jahn, Alexandra (author) Holland, Marika M. (author) Kay, Jennifer E. (author) Fasullo, John (author) Lamarque, Jean-François (author) Tilmes, Simone (author) Hannay, Cécile (author) Mills, Michael J. (author) Bailey, David A. (author) Barrett, Andrew P. (author) 2022-07-29 https://doi.org/10.1126/sciadv.abo2405 en eng Science Advances--Sci. Adv.--2375-2548 Supplemental data of Global Carbon Project 2019--10.18160/gcp-2019 CESM2 40-70N Biomass Emissions Homogenization Sensitivity Tests--10.5065/7f7c-zw94 NCAR Command Language (NCL)--10.5065/D6WD3XH5 articles:25613 doi:10.1126/sciadv.abo2405 ark:/85065/d7r49vj8 Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. article Text 2022 ftncar https://doi.org/10.1126/sciadv.abo2405 2024-03-21T18:00:26Z The mechanisms underlying decadal variability in Arctic sea ice remain actively debated. Here, we ability in boreal biomass burning (BB) emissions strongly influences simulated Arctic sea ice on multidecadal time scales. In particular, we find that a strong acceleration in sea ice decline in the early 21st century in the Community Earth System Model version 2 (CESM2) is related to increased variability in prescribed BB emissions in the sixth phase of the Coupled Model Intercomparison Project (CMIP6) through summertime aerosol-cloud interactions. Furthermore, we find that more than half of the reported improvement in sea ice sensitivity to CO2 emissions and global warming from CMIP5 to CMIP6 can be attributed to the increased BB variability, at least in the CESM. These results highlight a new kind of uncertainty that needs to be considered when incorporating new observational data into model forcing while also raising questions about the role of BB emissions on the observed Arctic sea ice loss. 1844590 1852977 AGS-1419571 Article in Journal/Newspaper Arctic Global warming Sea ice OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Science Advances 8 30
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description The mechanisms underlying decadal variability in Arctic sea ice remain actively debated. Here, we ability in boreal biomass burning (BB) emissions strongly influences simulated Arctic sea ice on multidecadal time scales. In particular, we find that a strong acceleration in sea ice decline in the early 21st century in the Community Earth System Model version 2 (CESM2) is related to increased variability in prescribed BB emissions in the sixth phase of the Coupled Model Intercomparison Project (CMIP6) through summertime aerosol-cloud interactions. Furthermore, we find that more than half of the reported improvement in sea ice sensitivity to CO2 emissions and global warming from CMIP5 to CMIP6 can be attributed to the increased BB variability, at least in the CESM. These results highlight a new kind of uncertainty that needs to be considered when incorporating new observational data into model forcing while also raising questions about the role of BB emissions on the observed Arctic sea ice loss. 1844590 1852977 AGS-1419571
author2 DeRepentigny, Patricia (author)
Jahn, Alexandra (author)
Holland, Marika M. (author)
Kay, Jennifer E. (author)
Fasullo, John (author)
Lamarque, Jean-François (author)
Tilmes, Simone (author)
Hannay, Cécile (author)
Mills, Michael J. (author)
Bailey, David A. (author)
Barrett, Andrew P. (author)
format Article in Journal/Newspaper
title Enhanced simulated early 21st century Arctic sea ice loss due to CMIP6 biomass burning emissions
spellingShingle Enhanced simulated early 21st century Arctic sea ice loss due to CMIP6 biomass burning emissions
title_short Enhanced simulated early 21st century Arctic sea ice loss due to CMIP6 biomass burning emissions
title_full Enhanced simulated early 21st century Arctic sea ice loss due to CMIP6 biomass burning emissions
title_fullStr Enhanced simulated early 21st century Arctic sea ice loss due to CMIP6 biomass burning emissions
title_full_unstemmed Enhanced simulated early 21st century Arctic sea ice loss due to CMIP6 biomass burning emissions
title_sort enhanced simulated early 21st century arctic sea ice loss due to cmip6 biomass burning emissions
publishDate 2022
url https://doi.org/10.1126/sciadv.abo2405
geographic Arctic
geographic_facet Arctic
genre Arctic
Global warming
Sea ice
genre_facet Arctic
Global warming
Sea ice
op_relation Science Advances--Sci. Adv.--2375-2548
Supplemental data of Global Carbon Project 2019--10.18160/gcp-2019
CESM2 40-70N Biomass Emissions Homogenization Sensitivity Tests--10.5065/7f7c-zw94
NCAR Command Language (NCL)--10.5065/D6WD3XH5
articles:25613
doi:10.1126/sciadv.abo2405
ark:/85065/d7r49vj8
op_rights Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
op_doi https://doi.org/10.1126/sciadv.abo2405
container_title Science Advances
container_volume 8
container_issue 30
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