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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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 |
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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/ uneingeschränkt info:eu-repo/semantics/restrictedAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/egusphere-2022-976 |
_version_ |
1766195157593489408 |