Design and results of the ice sheet model initialisation initMIP-Greenland: an ISMIP6 intercomparison

被引:93
|
作者
Goelzer, Heiko [1 ,2 ]
Nowicki, Sophie [3 ]
Edwards, Tamsin [4 ,28 ]
Beckley, Matthew [3 ]
Abe-Ouchi, Ayako [5 ]
Aschwanden, Andy [6 ]
Calov, Reinhard [7 ]
Gagliardini, Olivier [8 ]
Gillet-Chaulet, Fabien [8 ]
Golledge, Nicholas R. [9 ]
Gregory, Jonathan [10 ,11 ]
Greve, Ralf [12 ]
Humbert, Angelika [13 ,14 ]
Huybrechts, Philippe [15 ]
Kennedy, Joseph H. [16 ,17 ]
Larour, Eric [18 ]
Lipscomb, William H. [19 ,20 ]
Le Clec'h, Sebastien [21 ]
Lee, Victoria [22 ]
Morlighem, Mathieu [23 ]
Pattyn, Frank [2 ]
Payne, Antony J. [22 ]
Rodehacke, Christian [13 ,24 ]
Rueckamp, Martin [13 ]
Saito, Fuyuki [25 ]
Schlegel, Nicole [18 ]
Seroussi, Helene [18 ]
Shepherd, Andrew [26 ]
Sun, Sainan [2 ]
van de Wal, Roderik [1 ]
Ziemen, Florian A. [27 ]
机构
[1] Univ Utrecht, Inst Marine & Atmospher Res IMAU, Utrecht, Netherlands
[2] Univ Libre Bruxelles, Lab Glaciol, Brussels, Belgium
[3] NASA, GSFC, Cryospher Sci Branch, Greenbelt, MD USA
[4] Open Univ, Sch Environm Earth & Ecosyst Sci, Milton Keynes, Bucks, England
[5] Univ Tokyo, Atmosphere Ocean Res Inst, Kashiwa, Chiba, Japan
[6] Univ Alaska Fairbanks, Geophys Inst, Fairbanks, AK USA
[7] Potsdam Inst Climate Impact Res, Potsdam, Germany
[8] Univ Grenoble Alpes, CNRS, IRD, Grenoble INP,IGE, F-38000 Grenoble, France
[9] Victoria Univ Wellington, Antarctic Res Ctr, Wellington, New Zealand
[10] Univ Reading, Dept Meteorol, Reading, Berks, England
[11] Met Off Hadley Ctr, Exeter, Devon, England
[12] Hokkaido Univ, Inst Low Temp Sci, Sapporo, Hokkaido, Japan
[13] Alfred Wegener Inst Polar & Marine Res, Bremerhaven, Germany
[14] Univ Bremen, Bremen, Germany
[15] Vrije Univ Brussel, Brussels, Belgium
[16] Oak Ridge Natl Lab, Climate Change Sci Inst, Oak Ridge, TN USA
[17] Oak Ridge Natl Lab, Computat Sci & Engn Div, Oak Ridge, TN USA
[18] CALTECH, Jet Prop Lab, Pasadena, CA USA
[19] Los Alamos Natl Lab, Los Alamos, NM USA
[20] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
[21] CEA CNRS UVSQ, Lab Sci Climat & Environm, LSCE IPSL, Gif Sur Yvette, France
[22] Univ Bristol, Bristol, Avon, England
[23] Univ Calif Irvine, Irvine, CA USA
[24] Danish Meteorol Inst, Copenhagen, Denmark
[25] Japan Agcy Marine Earth Sci & Technol, Yokohama, Kanagawa, Japan
[26] Univ Leeds, Sch Earth & Environm, Leeds, W Yorkshire, England
[27] Max Planck Inst Meteorol, Hamburg, Germany
[28] Kings Coll London, Dept Geog, London, England
来源
CRYOSPHERE | 2018年 / 12卷 / 04期
基金
比利时弗兰德研究基金会; 欧洲研究理事会; 美国国家科学基金会; 日本学术振兴会;
关键词
SURFACE MASS-BALANCE; FUTURE SEA-LEVEL; HEAT-FLUX; SPATIAL SENSITIVITIES; ENVIRONMENTAL-CHANGE; ELEVATION FEEDBACK; OUTLET GLACIERS; CLIMATE; PROJECT; RESOLUTION;
D O I
10.5194/tc-12-1433-2018
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
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 this 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); they 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.
引用
收藏
页码:1433 / 1460
页数:28
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