Greater committed warming after accounting for the pattern effect

Our planet’s energy balance is sensitive to spatial inhomogeneities in sea surface temperature and sea ice changes, but this is typically ignored in climate projections. Here, we show the energy budget during recent decades can be closed by combining changes in effective radiative forcing, linear ra...

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Published in:Nature Climate Change
Main Authors: Zhou, Chen, Zelinka, Mark D., Dessler, Andrew E., Wang, Minghuai
Language:unknown
Published: 2022
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1755848
https://www.osti.gov/biblio/1755848
https://doi.org/10.1038/s41558-020-00955-x
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spelling ftosti:oai:osti.gov:1755848 2023-07-30T04:06:46+02:00 Greater committed warming after accounting for the pattern effect Zhou, Chen Zelinka, Mark D. Dessler, Andrew E. Wang, Minghuai 2022-01-04 application/pdf http://www.osti.gov/servlets/purl/1755848 https://www.osti.gov/biblio/1755848 https://doi.org/10.1038/s41558-020-00955-x unknown http://www.osti.gov/servlets/purl/1755848 https://www.osti.gov/biblio/1755848 https://doi.org/10.1038/s41558-020-00955-x doi:10.1038/s41558-020-00955-x 58 GEOSCIENCES 2022 ftosti https://doi.org/10.1038/s41558-020-00955-x 2023-07-11T10:00:08Z Our planet’s energy balance is sensitive to spatial inhomogeneities in sea surface temperature and sea ice changes, but this is typically ignored in climate projections. Here, we show the energy budget during recent decades can be closed by combining changes in effective radiative forcing, linear radiative damping and this pattern effect. The pattern effect is of comparable magnitude but opposite sign to Earth’s net energy imbalance in the 2000s, indicating its importance when predicting the future climate on the basis of observations. Additionally, after the pattern effect is accounted for, the best-estimate value of committed global warming at present-day forcing rises from 1.31 K (0.99–2.33 K, 5th–95th percentile) to over 2 K, and committed warming in 2100 with constant long-lived forcing increases from 1.32 K (0.94–2.03 K) to over 1.5 K, although the magnitude is sensitive to sea surface temperature dataset. Further constraints on the pattern effect are needed to reduce climate projection uncertainty. Other/Unknown Material Sea ice SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Nature Climate Change 11 2 132 136
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 58 GEOSCIENCES
spellingShingle 58 GEOSCIENCES
Zhou, Chen
Zelinka, Mark D.
Dessler, Andrew E.
Wang, Minghuai
Greater committed warming after accounting for the pattern effect
topic_facet 58 GEOSCIENCES
description Our planet’s energy balance is sensitive to spatial inhomogeneities in sea surface temperature and sea ice changes, but this is typically ignored in climate projections. Here, we show the energy budget during recent decades can be closed by combining changes in effective radiative forcing, linear radiative damping and this pattern effect. The pattern effect is of comparable magnitude but opposite sign to Earth’s net energy imbalance in the 2000s, indicating its importance when predicting the future climate on the basis of observations. Additionally, after the pattern effect is accounted for, the best-estimate value of committed global warming at present-day forcing rises from 1.31 K (0.99–2.33 K, 5th–95th percentile) to over 2 K, and committed warming in 2100 with constant long-lived forcing increases from 1.32 K (0.94–2.03 K) to over 1.5 K, although the magnitude is sensitive to sea surface temperature dataset. Further constraints on the pattern effect are needed to reduce climate projection uncertainty.
author Zhou, Chen
Zelinka, Mark D.
Dessler, Andrew E.
Wang, Minghuai
author_facet Zhou, Chen
Zelinka, Mark D.
Dessler, Andrew E.
Wang, Minghuai
author_sort Zhou, Chen
title Greater committed warming after accounting for the pattern effect
title_short Greater committed warming after accounting for the pattern effect
title_full Greater committed warming after accounting for the pattern effect
title_fullStr Greater committed warming after accounting for the pattern effect
title_full_unstemmed Greater committed warming after accounting for the pattern effect
title_sort greater committed warming after accounting for the pattern effect
publishDate 2022
url http://www.osti.gov/servlets/purl/1755848
https://www.osti.gov/biblio/1755848
https://doi.org/10.1038/s41558-020-00955-x
genre Sea ice
genre_facet Sea ice
op_relation http://www.osti.gov/servlets/purl/1755848
https://www.osti.gov/biblio/1755848
https://doi.org/10.1038/s41558-020-00955-x
doi:10.1038/s41558-020-00955-x
op_doi https://doi.org/10.1038/s41558-020-00955-x
container_title Nature Climate Change
container_volume 11
container_issue 2
container_start_page 132
op_container_end_page 136
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