Articles | Volume 11, issue 11
https://doi.org/10.5194/gmd-11-4657-2018
https://doi.org/10.5194/gmd-11-4657-2018
Development and technical paper
 | 
22 Nov 2018
Development and technical paper |  | 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

Constantijn J. Berends, Bas de Boer, and Roderik S. W. van de Wal

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Present-day mass loss rates are a precursor for West Antarctic Ice Sheet collapse
Tim van den Akker, William H. Lipscomb, Gunter R. Leguy, Jorjo Bernales, Constantijn J. Berends, Willem Jan van de Berg, and Roderik S. W. van de Wal
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Brief communication: velocities and thinning rates for Halfar’s analytical solution to the Shallow Ice Approximation
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CO2 and summer insolation as drivers for the Mid-Pleistocene transition
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Late Pleistocene glacial terminations accelerated by proglacial lakes
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The Utrecht Finite Volume Ice-Sheet Model (UFEMISM version 2.0) – part 1: description and idealised experiments
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Cited articles

Abe-Ouchi, A., Saito, F., Kawamura, K., Raymo, M. E., Okuno, J., Takahashi, K., and Blatter, H.: Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume, Nature Letters 500, 190–194, 2013. 
Alley, R. B.: The Younger Dryas cold interval as viewed from central Greenland, Quaternary Sci. Rev., 19, 213–226, 2000. 
Annan, J. D. and Hargreaves, J. C.: A new global reconstruction of temperature changes at the Last Glacial Maximum, Clim. Past, 9, 367–376, https://doi.org/10.5194/cp-9-367-2013, 2013. 
Bamber, J. L., Riva, R. E. M., Vermeersen, B. L. A., and LeBrocq, A. M.: Reassessment of the potential sea-level rise from a collapse of the West Antarctic Ice Sheet, Science, 324, 901–903, 2009. 
Berends, C., de Boer, B., and van de Wal, R.: Berends_etal_2018_GMD_supplement, [Data set], https://doi.org/10.5194/gmd-2018-145supplement, 2018a. 
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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.
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