Articles | Volume 11, issue 11
Geosci. Model Dev., 11, 4657–4675, 2018
https://doi.org/10.5194/gmd-11-4657-2018
Geosci. Model Dev., 11, 4657–4675, 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 et al.

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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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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.