Model-based changes in global annual mean surface temperature change (Delta T_g) and radiative forcing due to land ice albedo changes (Delta R_[LI]) over the last 5 Myr, supplementary material ...
It is still an open question how equilibrium warming in response to increasing radiative forcing – the specific equilibrium climate sensitivity S – depends on background climate. We here present palaeodata-based evidence on the state dependency of S, by using CO2 proxy data together with a 3-D ice-s...
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ftdatacite:10.1594/pangaea.855449 2024-09-09T19:45:10+00:00 Model-based changes in global annual mean surface temperature change (Delta T_g) and radiative forcing due to land ice albedo changes (Delta R_[LI]) over the last 5 Myr, supplementary material ... Köhler, Peter de Boer, Bas von der Heydt, Anna S Stap, Lennert Bastiaan van de Wal, Roderik S W 2015 application/zip https://dx.doi.org/10.1594/pangaea.855449 https://doi.pangaea.de/10.1594/PANGAEA.855449 en eng PANGAEA https://dx.doi.org/10.5194/cp-11-1801-2015 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 dataset Supplementary Dataset Dataset 2015 ftdatacite https://doi.org/10.1594/pangaea.85544910.5194/cp-11-1801-2015 2024-08-01T10:51:31Z It is still an open question how equilibrium warming in response to increasing radiative forcing – the specific equilibrium climate sensitivity S – depends on background climate. We here present palaeodata-based evidence on the state dependency of S, by using CO2 proxy data together with a 3-D ice-sheet-model-based reconstruction of land ice albedo over the last 5 million years (Myr). We find that the land ice albedo forcing depends non-linearly on the background climate, while any non-linearity of CO2 radiative forcing depends on the CO2 data set used. This non-linearity has not, so far, been accounted for in similar approaches due to previously more simplistic approximations, in which land ice albedo radiative forcing was a linear function of sea level change. The latitudinal dependency of ice-sheet area changes is important for the non-linearity between land ice albedo and sea level. In our set-up, in which the radiative forcing of CO2 and of the land ice albedo (LI) is combined, we find a state ... : With an inverse climate model setup, that include 3D-ice sheet models, the benthic d18O global stack LR04 of the last 5 Myr (Lisiecki and Raymo, 2005, doi:10.1029/2004PA001071) was in a previous study (de Boer et al., 2014, doi:10.1038/ncomms3999) deconvolved into a temperature component and a sea level (ice sheet) component. The calculated changes in land ice area (as function of time and latitude) combined with incoming solar radiation (Laskar et al., 2004, doi:10.1051/0004-6361:20041335) and a simplified energy balance scheme (Köhler et al., 2010, doi:10.1016/j.quascirev.2009.09.026) are used to calculate changes in radiative forcing due to land ice albedo changes (Delta R_[LI]) over the last 5 Myr (changes normalized to global changes in radiative forcing, units: W/m^2). Three different assumptions on polar amplification are then used to calculate out of the model-based changes in temperature over the northern hemispheric land ice sheets (related to deep ocean temperature and derived from the ... Dataset Ice Sheet DataCite |
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Open Polar |
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ftdatacite |
language |
English |
description |
It is still an open question how equilibrium warming in response to increasing radiative forcing – the specific equilibrium climate sensitivity S – depends on background climate. We here present palaeodata-based evidence on the state dependency of S, by using CO2 proxy data together with a 3-D ice-sheet-model-based reconstruction of land ice albedo over the last 5 million years (Myr). We find that the land ice albedo forcing depends non-linearly on the background climate, while any non-linearity of CO2 radiative forcing depends on the CO2 data set used. This non-linearity has not, so far, been accounted for in similar approaches due to previously more simplistic approximations, in which land ice albedo radiative forcing was a linear function of sea level change. The latitudinal dependency of ice-sheet area changes is important for the non-linearity between land ice albedo and sea level. In our set-up, in which the radiative forcing of CO2 and of the land ice albedo (LI) is combined, we find a state ... : With an inverse climate model setup, that include 3D-ice sheet models, the benthic d18O global stack LR04 of the last 5 Myr (Lisiecki and Raymo, 2005, doi:10.1029/2004PA001071) was in a previous study (de Boer et al., 2014, doi:10.1038/ncomms3999) deconvolved into a temperature component and a sea level (ice sheet) component. The calculated changes in land ice area (as function of time and latitude) combined with incoming solar radiation (Laskar et al., 2004, doi:10.1051/0004-6361:20041335) and a simplified energy balance scheme (Köhler et al., 2010, doi:10.1016/j.quascirev.2009.09.026) are used to calculate changes in radiative forcing due to land ice albedo changes (Delta R_[LI]) over the last 5 Myr (changes normalized to global changes in radiative forcing, units: W/m^2). Three different assumptions on polar amplification are then used to calculate out of the model-based changes in temperature over the northern hemispheric land ice sheets (related to deep ocean temperature and derived from the ... |
format |
Dataset |
author |
Köhler, Peter de Boer, Bas von der Heydt, Anna S Stap, Lennert Bastiaan van de Wal, Roderik S W |
spellingShingle |
Köhler, Peter de Boer, Bas von der Heydt, Anna S Stap, Lennert Bastiaan van de Wal, Roderik S W Model-based changes in global annual mean surface temperature change (Delta T_g) and radiative forcing due to land ice albedo changes (Delta R_[LI]) over the last 5 Myr, supplementary material ... |
author_facet |
Köhler, Peter de Boer, Bas von der Heydt, Anna S Stap, Lennert Bastiaan van de Wal, Roderik S W |
author_sort |
Köhler, Peter |
title |
Model-based changes in global annual mean surface temperature change (Delta T_g) and radiative forcing due to land ice albedo changes (Delta R_[LI]) over the last 5 Myr, supplementary material ... |
title_short |
Model-based changes in global annual mean surface temperature change (Delta T_g) and radiative forcing due to land ice albedo changes (Delta R_[LI]) over the last 5 Myr, supplementary material ... |
title_full |
Model-based changes in global annual mean surface temperature change (Delta T_g) and radiative forcing due to land ice albedo changes (Delta R_[LI]) over the last 5 Myr, supplementary material ... |
title_fullStr |
Model-based changes in global annual mean surface temperature change (Delta T_g) and radiative forcing due to land ice albedo changes (Delta R_[LI]) over the last 5 Myr, supplementary material ... |
title_full_unstemmed |
Model-based changes in global annual mean surface temperature change (Delta T_g) and radiative forcing due to land ice albedo changes (Delta R_[LI]) over the last 5 Myr, supplementary material ... |
title_sort |
model-based changes in global annual mean surface temperature change (delta t_g) and radiative forcing due to land ice albedo changes (delta r_[li]) over the last 5 myr, supplementary material ... |
publisher |
PANGAEA |
publishDate |
2015 |
url |
https://dx.doi.org/10.1594/pangaea.855449 https://doi.pangaea.de/10.1594/PANGAEA.855449 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
https://dx.doi.org/10.5194/cp-11-1801-2015 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.85544910.5194/cp-11-1801-2015 |
_version_ |
1809914802003247104 |