Description of historical and future projection simulations by the global coupled E3SMv1.0 model as used in CMIP6
Abstract ∼ 11 to ∼ 6 Sv (Sverdrup) relative to other CMIP6 models. The sea ice, especially in the Northern Hemisphere, decreases rapidly with large seasonal variability. We detect a significant polar amplification in E3SMv1.0 from the atmosphere, ocean, and sea ice. Comparing the SSP5-8.5 all-forcing experiment with the GHG-only experiment, we find that the unmasking of the aerosol effects due to the decline of the aerosol loading in the future projection period causes transient accelerated warming in the all-forcing experiment in the first half of the 21st century. While the oceanic climate response is mainly controlled by the GHG forcing, the land runoff response is impacted primarily by forcings other than GHG over certain regions, e.g., southern North America, southern Africa, central Africa, and eastern Asia. However, the importance of the GHG forcing on the land runoff changes grows in the future climate projection period compared to the historical period.
- Standort
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Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
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Online-Ressource
- Sprache
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Englisch
- Erschienen in
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Description of historical and future projection simulations by the global coupled E3SMv1.0 model as used in CMIP6 ; volume:15 ; number:9 ; year:2022 ; pages:3941-3967 ; extent:27
Geoscientific model development ; 15, Heft 9 (2022), 3941-3967 (gesamt 27)
- Urheber
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Zheng, Xue
Li, Qing
Zhou, Tian
Tang, Qi
Van Roekel, Luke P.
Golaz, Jean-Christophe
Wang, Hailong
Cameron-Smith, Philip
- DOI
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10.5194/gmd-15-3941-2022
- URN
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urn:nbn:de:101:1-2022051905364564589596
- Rechteinformation
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
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15.08.2025, 07:29 MESZ
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Beteiligte
- Zheng, Xue
- Li, Qing
- Zhou, Tian
- Tang, Qi
- Van Roekel, Luke P.
- Golaz, Jean-Christophe
- Wang, Hailong
- Cameron-Smith, Philip
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