Greenland Surface Mass Balance as Simulated by the Community Earth System Model. Part I: Model Evaluation and 1850–2005 Results

Vizcaíno, Miren; Lipscomb, William H.; Sacks, William J.; van Angelen, Jan H.; Wouters, Bert; van den Broeke, Michiel R.

doi:10.1175/jcli-d-12-00615.1

Title: Greenland Surface Mass Balance as Simulated by the Community Earth System Model. Part I: Model Evaluation and 1850–2005 Results

Journal Article · Fri Oct 04 00:00:00 EDT 2013 · Journal of Climate

DOI:https://doi.org/10.1175/jcli-d-12-00615.1· OSTI ID:1565233

Vizcaíno, Miren ^[1]; Lipscomb, William H. ^[2]; Sacks, William J. ^[3]; van Angelen, Jan H. ^[1]; Wouters, Bert ^[4]; van den Broeke, Michiel R. ^[1]

Utrecht Univ., Utrecht (Netherlands). Inst. for Marine and Atmospheric Research; Univ. of California, Berkeley, CA (United States). Dept. of Geography
Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
National Center for Atmospheric Research, Boulder, CO (United States)
Univ. of Colorado, Boulder, CO (United States). Dept. of Physics; Bristol Univ. (United Kingdom). Bristol Glaciology Centre, School of Geographical Sciences

The modeling of the surface mass balance (SMB) of the Greenland Ice Sheet (GIS) requires high-resolution models in order to capture the observed large gradients in the steep marginal areas. Until now, global climate models have not been considered suitable to model ice sheet SMB owing to model biases and insufficient resolution. This study analyzes the GIS SMB simulated for the period 1850–2005 by the Community Earth System Model (CESM), which includes a new ice sheet component with multiple elevation classes for SMB calculations. The model is evaluated against observational data and output from the regional model Regional Atmospheric Climate Model version 2 (RACMO2). Because of a lack of major climate biases, a sophisticated calculation of snow processes (including surface albedo evolution) and an adequate downscaling technique, CESM is able to realistically simulate GIS surface climate and SMB. CESM SMB agrees reasonably well with in situ data from 475 locations ($$r$$ = 0.80) and output from RACMO2 ($$r$$ = 0.79). The simulated mean SMB for 1960–2005 is 359 ± 120 Gt yr^-1 in the range of estimates from regional climate models. The simulated seasonal mass variability is comparable with mass observations from the Gravity Recovery and Climate Experiment (GRACE), with synchronous annual maximum (May) and minimum (August–September) and similar amplitudes of the seasonal cycle. CESM is able to simulate the bands of precipitation maxima along the southeast and northwest margins, but absolute precipitation rates are underestimated along the southeastern margin and overestimated in the high interior. The model correctly simulates the major ablation areas. Total refreezing represents 35% of the available liquid water (the sum of rain and melt).

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Research Organization:: Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States). Oak Ridge Leadership Computing Facility (OLCF); UT-Battelle LLC/ORNL, Oak Ridge, TN (United States); Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)

Sponsoring Organization:: USDOE Office of Science (SC)

Grant/Contract Number:: AC05-00OR22725; AC52-06NA25396

OSTI ID:: 1565233

Journal Information:: Journal of Climate, Vol. 26, Issue 20; ISSN 0894-8755

Publisher:: American Meteorological SocietyCopyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 49 works

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