Print Email Facebook Twitter Present-Day Greenland Ice Sheet Climate and Surface Mass Balance in CESM2 Title Present-Day Greenland Ice Sheet Climate and Surface Mass Balance in CESM2 Author van Kampenhout, Leonardus (Universiteit Utrecht) Lenaerts, Jan T.M. (University of Colorado) Lipscomb, William H. (National Center for Atmospheric Research) Lhermitte, S.L.M. (TU Delft Mathematical Geodesy and Positioning) Noël, Brice (Universiteit Utrecht) Vizcaino, M. (TU Delft Physical and Space Geodesy) Sacks, W. J. (National Center for Atmospheric Research) van den Broeke, Michiel R. (Universiteit Utrecht) Date 2020 Abstract The response of the Greenland Ice Sheet (GrIS) to a warmer climate is uncertain on long time scales. Climate models, such as those participating in the Coupled Model Intercomparison Project phase 6 (CMIP6), are used to assess this uncertainty. The Community Earth System Model version 2.1 (CESM2) is a CMIP6 model capable of running climate simulations with either one-way coupling (fixed ice sheet geometry) or two-way coupling (dynamic geometry) to the GrIS. The model features prognostic snow albedo, online downscaling using elevation classes, and a firn pack to refreeze percolating melt water. Here we evaluate the representation of the GrIS surface energy balance and surface mass balance in CESM2 at 1° resolution with fixed GrIS geometry. CESM2 agrees closely with ERA-Interim reanalysis data for key controls on GrIS SMB: surface pressure, sea ice extent, 500 hPa geopotential height, wind speed, and 700 hPa air temperature. Cloudsat-CALIPSO data show that supercooled liquid-containing clouds are adequately represented, whereas comparisons to Moderate Resolution Imaging Spectroradiometer and CM SAF Cloud, Albedo, and Surface Radiation data set from Advanced Very High Resolution Radiometer data second edition data suggest that CESM2 underestimates surface albedo. The seasonal cycle and spatial patterns of surface energy balance and surface mass balance components in CESM2 agree well with regional climate model RACMO2.3p2, with GrIS-integrated melt, refreezing, and runoff bracketed by RACMO2 counterparts at 11 and 1 km. Time series of melt, runoff, and SMB show a break point around 1990, similar to RACMO2. These results suggest that GrIS SMB is realistic in CESM2, which adds confidence to coupled ice sheet-climate experiments that aim to assess the GrIS contribution to future sea level rise. Subject CESM2ESMGCMGreenlandice sheetssurface mass balance To reference this document use: http://resolver.tudelft.nl/uuid:c18757ff-4cd2-4abb-a306-975395f8d5ff DOI https://doi.org/10.1029/2019JF005318 ISSN 2169-9003 Source Journal of Geophysical Research: Earth Surface, 125 (2), 1-25 Part of collection Institutional Repository Document type journal article Rights © 2020 Leonardus van Kampenhout, Jan T.M. Lenaerts, William H. Lipscomb, S.L.M. Lhermitte, Brice Noël, M. Vizcaino, W. J. Sacks, Michiel R. van den Broeke Files PDF Kampenhout_et_al_2020_Jou ... urface.pdf 52.26 MB Close viewer /islandora/object/uuid:c18757ff-4cd2-4abb-a306-975395f8d5ff/datastream/OBJ/view