Design and results of the ice sheet model initialisation experiments initMIP-Greenland: an ISMIP6 intercomparison.
Heiko Goelzer, Sophie Nowicki, Tamsin Edwards, Matthew Beckley, Ayako Abe-Ouchi, Andy Aschwanden, Reinhard Calov, Olivier Gagliardini, Fabien Gillet-Chaulet, Nicholas R Golledge, Jonathan Gregory, Ralf Greve, Angelika Humbert, Philippe Huybrechts, Joseph H Kennedy, Eric Larour, William H Lipscomb, Sébastien Le Clećh, Victoria Lee, Mathieu Morlighem, Frank Pattyn, Antony J Payne, Christian Rodehacke, Martin Rückamp, Fuyuki Saito, Nicole Schlegel, Helene Seroussi, Andrew Shepherd, Sainan Sun, Roderik van de Wal, Florian A Ziemen
Author Information
Heiko Goelzer: Utrecht University, Institute for Marine and Atmospheric Research (IMAU), Utrecht, Netherlands.
Sophie Nowicki: NASA GSFC, Cryospheric Sciences Branch, Greenbelt, USA.
Tamsin Edwards: School of Environment, Earth & Ecosystem Sciences, The Open University, Milton Keynes, United Kingdom.
Matthew Beckley: NASA GSFC, Cryospheric Sciences Branch, Greenbelt, USA.
Ayako Abe-Ouchi: Atmosphere Ocean Research Institute, University of Tokyo, Kashiwa, Japan.
Andy Aschwanden: Geophysical Institute, University of Alaska Fairbanks, USA.
Reinhard Calov: Potsdam Institute for Climate Impact Research, Potsdam, Germany.
Earlier large-scale Greenland ice sheet sea-level projections (e.g., those run during the ice2sea and SeaRISE initiatives) have shown that ice sheet initial conditions have a large effect on the projections and give rise to important uncertainties. The goal of the initMIP-Greenland intercomparison exercise is to compare, evaluate and improve the initialisation techniques used in the ice sheet modelling community and to estimate the associated uncertainties in modelled mass changes. initMIP-Greenland is the first in a series of ice sheet model intercomparison activities within ISMIP6 (the Ice Sheet Model Intercomparison Project for CMIP6), which is the primary activity within the Coupled Model Intercomparison Project - phase 6 (CMIP6) focusing on the ice sheets. Two experiments for the large-scale Greenland ice sheet have been designed to allow intercomparison between participating models of 1) the initial present-day state of the ice sheet and 2) the response in two idealised forward experiments. The forward experiments serve to evaluate the initialisation in terms of model drift (forward run without additional forcing) and in response to a large perturbation (prescribed surface mass balance anomaly), and should not be interpreted as sea-level projections. We present and discuss results that highlight the diversity of data sets, boundary conditions and initialisation techniques used in the community to generate initial states of the Greenland ice sheet. We find good agreement across the ensemble for the dynamic response to surface mass balance changes in areas where the simulated ice sheets overlap, but differences arising from the initial size of the ice sheet. The model drift in the control experiment is reduced for models that participated in earlier intercomparison exercises.
References
Proc Natl Acad Sci U S A. 2011 May 31;108(22):8978-83
[PMID: 21576500]
Geosci Model Dev. 2016;9(12):4521-4545
[PMID: 29697697]
J Geophys Res Earth Surf. 2015 Feb;120(2):212-241
[PMID: 26213664]
Proc Natl Acad Sci U S A. 2013 Aug 27;110(35):14156-61
[PMID: 23940337]