Abstract
Abstract. On multi-million-year timescales, fully coupled ice sheet–climate simulations are hampered by computational limitations, even at
coarser resolutions and when using asynchronous coupling schemes. In this
study, a novel coupling method CLISEMv1.0 (CLimate–Ice Sheet EMulator
version 1.0) is presented, where a Gaussian process emulator is applied to
the climate model HadSM3 and coupled to the ice sheet model AISMPALEO. The
temperature and precipitation fields from HadSM3 are emulated to feed the
mass balance model in AISMPALEO. The sensitivity of the evolution of the ice sheet over time is tested with respect to the number of predefined ice sheet
geometries that the emulator is calibrated on. Additionally, the model
performance is evaluated in terms of the formulation of the ice sheet parameter
(being ice sheet volume, ice sheet area or both) and the
coupling time. Sensitivity experiments are conducted to explore the
uncertainty introduced by the emulator. In addition, different lapse rate
adjustments are used between the relatively coarse climate model and the
much finer ice sheet model topography. It is shown that the ice sheet
evolution over a million-year timescale is strongly sensitive to the
definition of the ice sheet parameter and to the number of predefined ice
sheet geometries. With the new coupling procedure, we provide a
computationally efficient framework for simulating ice sheet–climate
interactions on a multi-million-year timescale that allows for a large
number of sensitivity tests.
Funder
Fonds De La Recherche Scientifique - FNRS
Cited by
3 articles.
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