Articles | Volume 11, issue 11
https://doi.org/10.5194/gmd-11-4657-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-11-4657-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Development and technical paper
| 
22 Nov 2018
Development and technical paper |
| 22 Nov 2018
| 22 Nov 2018
Application of HadCM3@Bristolv1.0 simulations of paleoclimate as forcing for an ice-sheet model, ANICE2.1: set-up and benchmark experiments
Institute for Marine and Atmospheric research Utrecht, Utrecht
University, Utrecht, the Netherlands
Bas de Boer
Institute for Marine and Atmospheric research Utrecht, Utrecht
University, Utrecht, the Netherlands
Roderik S. W. van de Wal
Institute for Marine and Atmospheric research Utrecht, Utrecht
University, Utrecht, the Netherlands
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Cited
17 citations as recorded by crossref.
- Late Pleistocene glacial terminations accelerated by proglacial lakes M. Scherrenberg et al. 10.5194/cp-20-1761-2024
- Modeling Northern Hemispheric Ice Sheet Dynamics, Sea Level Change, and Solid Earth Deformation Through the Last Glacial Cycle H. Han et al. 10.1029/2020JF006040
- On the Cause of the Mid‐Pleistocene Transition C. Berends et al. 10.1029/2020RG000727
- Modelling ice sheet evolution and atmospheric CO<sub>2</sub> during the Late Pliocene C. Berends et al. 10.5194/cp-15-1603-2019
- Modelling feedbacks between the Northern Hemisphere ice sheets and climate during the last glacial cycle M. Scherrenberg et al. 10.5194/cp-19-399-2023
- Comparison and Synthesis of Sea‐Level and Deep‐Sea Temperature Variations Over the Past 40 Million Years E. Rohling et al. 10.1029/2022RG000775
- Benchmarking the vertically integrated ice-sheet model IMAU-ICE (version 2.0) C. Berends et al. 10.5194/gmd-15-5667-2022
- Net effect of ice-sheet–atmosphere interactions reduces simulated transient Miocene Antarctic ice-sheet variability L. Stap et al. 10.5194/tc-16-1315-2022
- The impact of icebergs of sub-Antarctic origin on Southern Ocean ice-rafted debris distributions G. Bigg 10.1016/j.quascirev.2020.106204
- Simulation of a fully coupled 3D glacial isostatic adjustment – ice sheet model for the Antarctic ice sheet over a glacial cycle C. van Calcar et al. 10.5194/gmd-16-5473-2023
- The Utrecht Finite Volume Ice-Sheet Model: UFEMISM (version 1.0) C. Berends et al. 10.5194/gmd-14-2443-2021
- Miocene Antarctic Ice Sheet area adapts significantly faster than volume to CO2-induced climate change L. Stap et al. 10.5194/cp-20-257-2024
- Reconciling Southern Ocean fronts equatorward migration with minor Antarctic ice volume change during Miocene cooling S. Hou et al. 10.1038/s41467-023-43106-4
- A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0 J. Van Breedam et al. 10.5194/gmd-14-6373-2021
- A stochastic parameterization of ice sheet surface mass balance for the Stochastic Ice-Sheet and Sea-Level System Model (StISSM v1.0) L. Ultee et al. 10.5194/gmd-17-1041-2024
- GrSMBMIP: intercomparison of the modelled 1980–2012 surface mass balance over the Greenland Ice Sheet X. Fettweis et al. 10.5194/tc-14-3935-2020
- Reconstructing the evolution of ice sheets, sea level, and atmospheric CO<sub>2</sub> during the past 3.6 million years C. Berends et al. 10.5194/cp-17-361-2021
17 citations as recorded by crossref.
- Late Pleistocene glacial terminations accelerated by proglacial lakes M. Scherrenberg et al. 10.5194/cp-20-1761-2024
- Modeling Northern Hemispheric Ice Sheet Dynamics, Sea Level Change, and Solid Earth Deformation Through the Last Glacial Cycle H. Han et al. 10.1029/2020JF006040
- On the Cause of the Mid‐Pleistocene Transition C. Berends et al. 10.1029/2020RG000727
- Modelling ice sheet evolution and atmospheric CO<sub>2</sub> during the Late Pliocene C. Berends et al. 10.5194/cp-15-1603-2019
- Modelling feedbacks between the Northern Hemisphere ice sheets and climate during the last glacial cycle M. Scherrenberg et al. 10.5194/cp-19-399-2023
- Comparison and Synthesis of Sea‐Level and Deep‐Sea Temperature Variations Over the Past 40 Million Years E. Rohling et al. 10.1029/2022RG000775
- Benchmarking the vertically integrated ice-sheet model IMAU-ICE (version 2.0) C. Berends et al. 10.5194/gmd-15-5667-2022
- Net effect of ice-sheet–atmosphere interactions reduces simulated transient Miocene Antarctic ice-sheet variability L. Stap et al. 10.5194/tc-16-1315-2022
- The impact of icebergs of sub-Antarctic origin on Southern Ocean ice-rafted debris distributions G. Bigg 10.1016/j.quascirev.2020.106204
- Simulation of a fully coupled 3D glacial isostatic adjustment – ice sheet model for the Antarctic ice sheet over a glacial cycle C. van Calcar et al. 10.5194/gmd-16-5473-2023
- The Utrecht Finite Volume Ice-Sheet Model: UFEMISM (version 1.0) C. Berends et al. 10.5194/gmd-14-2443-2021
- Miocene Antarctic Ice Sheet area adapts significantly faster than volume to CO2-induced climate change L. Stap et al. 10.5194/cp-20-257-2024
- Reconciling Southern Ocean fronts equatorward migration with minor Antarctic ice volume change during Miocene cooling S. Hou et al. 10.1038/s41467-023-43106-4
- A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0 J. Van Breedam et al. 10.5194/gmd-14-6373-2021
- A stochastic parameterization of ice sheet surface mass balance for the Stochastic Ice-Sheet and Sea-Level System Model (StISSM v1.0) L. Ultee et al. 10.5194/gmd-17-1041-2024
- GrSMBMIP: intercomparison of the modelled 1980–2012 surface mass balance over the Greenland Ice Sheet X. Fettweis et al. 10.5194/tc-14-3935-2020
- Reconstructing the evolution of ice sheets, sea level, and atmospheric CO<sub>2</sub> during the past 3.6 million years C. Berends et al. 10.5194/cp-17-361-2021
Latest update: 17 Nov 2024
Short summary
We have devised a novel way to couple a climate model to an ice-sheet model. Usually, climate models are too slow to simulate more than a few centuries, whereas our new model set-up can simulate a full 120 000-year ice age in about 12 h. This makes it possible to look at the interactions between global climate and ice sheets on long timescales, something which is relevant for both research into past climate and future projections.
We have devised a novel way to couple a climate model to an ice-sheet model. Usually, climate...
