Better constrained climate sensitivity when accounting for dataset dependency on pattern effect estimates

Equilibrium climate sensitivity (ECS) constrained based on the instrumental record of the historical warming becomes coherent with other lines evidence when the dependence of radiative feedbacks on the pattern of surface temperature change (pattern effect) is incorporated. Pattern effect strength is...

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Main Authors: Modak, Angshuman, Mauritsen, Thorsten
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2022-976
https://noa.gwlb.de/receive/cop_mods_00062838
https://egusphere.copernicus.org/preprints/egusphere-2022-976/egusphere-2022-976.pdf
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00062838 2023-05-15T18:18:33+02:00 Better constrained climate sensitivity when accounting for dataset dependency on pattern effect estimates Modak, Angshuman Mauritsen, Thorsten 2022-10 electronic https://doi.org/10.5194/egusphere-2022-976 https://noa.gwlb.de/receive/cop_mods_00062838 https://egusphere.copernicus.org/preprints/egusphere-2022-976/egusphere-2022-976.pdf eng eng Copernicus Publications https://doi.org/10.5194/egusphere-2022-976 https://noa.gwlb.de/receive/cop_mods_00062838 https://egusphere.copernicus.org/preprints/egusphere-2022-976/egusphere-2022-976.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/restrictedAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2022 ftnonlinearchiv https://doi.org/10.5194/egusphere-2022-976 2022-10-09T23:12:06Z Equilibrium climate sensitivity (ECS) constrained based on the instrumental record of the historical warming becomes coherent with other lines evidence when the dependence of radiative feedbacks on the pattern of surface temperature change (pattern effect) is incorporated. Pattern effect strength is usually estimated with atmosphere-only model simulations forced with observed historical sea-surface temperature (SST) and sea-ice change, and constant pre-industrial forcing. However, recent studies indicate that pattern effect estimates depend on the choice of SST boundary condition dataset, due to differences in the measurement sources and the techniques used to merge and construct them. Here, we systematically explore this dataset dependency by applying seven different observed SST datasets to the MPI-ESM1.2-LR model covering 1871–2017. We find that the pattern effect ranges from -0.01 ± 0.09 Wm-2 K-1 to 0.42 ± 0.10 Wm-2 K-1 (standard error), whereby the commonly used AMIPII dataset produces by far the largest estimate. When accounting for the generally weaker pattern effect in MPI-ESM1.2-LR compared to other models, as well as dataset dependency and inter-model spread, we obtain a combined pattern effect estimate of 0.30 Wm-2 K-1 [-0.14 to 0.74 Wm-2 K-1] (5–95 percentiles) and a resulting instrumental record ECS estimate of 3.1 K [1.7 to 9.2 K], which is slightly lower and better constrained than in previous studies. Article in Journal/Newspaper Sea ice Niedersächsisches Online-Archiv NOA
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Modak, Angshuman
Mauritsen, Thorsten
Better constrained climate sensitivity when accounting for dataset dependency on pattern effect estimates
topic_facet article
Verlagsveröffentlichung
description Equilibrium climate sensitivity (ECS) constrained based on the instrumental record of the historical warming becomes coherent with other lines evidence when the dependence of radiative feedbacks on the pattern of surface temperature change (pattern effect) is incorporated. Pattern effect strength is usually estimated with atmosphere-only model simulations forced with observed historical sea-surface temperature (SST) and sea-ice change, and constant pre-industrial forcing. However, recent studies indicate that pattern effect estimates depend on the choice of SST boundary condition dataset, due to differences in the measurement sources and the techniques used to merge and construct them. Here, we systematically explore this dataset dependency by applying seven different observed SST datasets to the MPI-ESM1.2-LR model covering 1871–2017. We find that the pattern effect ranges from -0.01 ± 0.09 Wm-2 K-1 to 0.42 ± 0.10 Wm-2 K-1 (standard error), whereby the commonly used AMIPII dataset produces by far the largest estimate. When accounting for the generally weaker pattern effect in MPI-ESM1.2-LR compared to other models, as well as dataset dependency and inter-model spread, we obtain a combined pattern effect estimate of 0.30 Wm-2 K-1 [-0.14 to 0.74 Wm-2 K-1] (5–95 percentiles) and a resulting instrumental record ECS estimate of 3.1 K [1.7 to 9.2 K], which is slightly lower and better constrained than in previous studies.
format Article in Journal/Newspaper
author Modak, Angshuman
Mauritsen, Thorsten
author_facet Modak, Angshuman
Mauritsen, Thorsten
author_sort Modak, Angshuman
title Better constrained climate sensitivity when accounting for dataset dependency on pattern effect estimates
title_short Better constrained climate sensitivity when accounting for dataset dependency on pattern effect estimates
title_full Better constrained climate sensitivity when accounting for dataset dependency on pattern effect estimates
title_fullStr Better constrained climate sensitivity when accounting for dataset dependency on pattern effect estimates
title_full_unstemmed Better constrained climate sensitivity when accounting for dataset dependency on pattern effect estimates
title_sort better constrained climate sensitivity when accounting for dataset dependency on pattern effect estimates
publisher Copernicus Publications
publishDate 2022
url https://doi.org/10.5194/egusphere-2022-976
https://noa.gwlb.de/receive/cop_mods_00062838
https://egusphere.copernicus.org/preprints/egusphere-2022-976/egusphere-2022-976.pdf
genre Sea ice
genre_facet Sea ice
op_relation https://doi.org/10.5194/egusphere-2022-976
https://noa.gwlb.de/receive/cop_mods_00062838
https://egusphere.copernicus.org/preprints/egusphere-2022-976/egusphere-2022-976.pdf
op_rights https://creativecommons.org/licenses/by/4.0/
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info:eu-repo/semantics/restrictedAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5194/egusphere-2022-976
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