Remapping of Greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections

Future sea-level change projections with process-based stand-alone ice sheet models are typically driven with surface mass balance (SMB) forcing derived from climate models. In this work we address the problems arising from a mismatch of the modelled ice sheet geometry with the geometry used by the...

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Published in:The Cryosphere
Main Authors: Goelzer, Heiko, Noël, Brice P. Y., Edwards, Tamsin L., Fettweis, Xavier, Gregory, Jonathan M., Lipscomb, William H., Wal, Roderik S. W., Broeke, Michiel R.
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-1747-2020
https://tc.copernicus.org/articles/14/1747/2020/
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spelling ftcopernicus:oai:publications.copernicus.org:tc79207 2023-05-15T16:27:53+02:00 Remapping of Greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections Goelzer, Heiko Noël, Brice P. Y. Edwards, Tamsin L. Fettweis, Xavier Gregory, Jonathan M. Lipscomb, William H. Wal, Roderik S. W. Broeke, Michiel R. 2020-06-02 application/pdf https://doi.org/10.5194/tc-14-1747-2020 https://tc.copernicus.org/articles/14/1747/2020/ eng eng doi:10.5194/tc-14-1747-2020 https://tc.copernicus.org/articles/14/1747/2020/ eISSN: 1994-0424 Text 2020 ftcopernicus https://doi.org/10.5194/tc-14-1747-2020 2020-07-20T16:22:07Z Future sea-level change projections with process-based stand-alone ice sheet models are typically driven with surface mass balance (SMB) forcing derived from climate models. In this work we address the problems arising from a mismatch of the modelled ice sheet geometry with the geometry used by the climate model. We present a method for applying SMB forcing from climate models to a wide range of Greenland ice sheet models with varying and temporally evolving geometries. In order to achieve that, we translate a given SMB anomaly field as a function of absolute location to a function of surface elevation for 25 regional drainage basins, which can then be applied to different modelled ice sheet geometries. The key feature of the approach is the non-locality of this remapping process. The method reproduces the original forcing data closely when remapped to the original geometry. When remapped to different modelled geometries it produces a physically meaningful forcing with smooth and continuous SMB anomalies across basin divides. The method considerably reduces non-physical biases that would arise by applying the SMB anomaly derived for the climate model geometry directly to a large range of modelled ice sheet model geometries. Text Greenland Ice Sheet Copernicus Publications: E-Journals Greenland The Cryosphere 14 6 1747 1762
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Future sea-level change projections with process-based stand-alone ice sheet models are typically driven with surface mass balance (SMB) forcing derived from climate models. In this work we address the problems arising from a mismatch of the modelled ice sheet geometry with the geometry used by the climate model. We present a method for applying SMB forcing from climate models to a wide range of Greenland ice sheet models with varying and temporally evolving geometries. In order to achieve that, we translate a given SMB anomaly field as a function of absolute location to a function of surface elevation for 25 regional drainage basins, which can then be applied to different modelled ice sheet geometries. The key feature of the approach is the non-locality of this remapping process. The method reproduces the original forcing data closely when remapped to the original geometry. When remapped to different modelled geometries it produces a physically meaningful forcing with smooth and continuous SMB anomalies across basin divides. The method considerably reduces non-physical biases that would arise by applying the SMB anomaly derived for the climate model geometry directly to a large range of modelled ice sheet model geometries.
format Text
author Goelzer, Heiko
Noël, Brice P. Y.
Edwards, Tamsin L.
Fettweis, Xavier
Gregory, Jonathan M.
Lipscomb, William H.
Wal, Roderik S. W.
Broeke, Michiel R.
spellingShingle Goelzer, Heiko
Noël, Brice P. Y.
Edwards, Tamsin L.
Fettweis, Xavier
Gregory, Jonathan M.
Lipscomb, William H.
Wal, Roderik S. W.
Broeke, Michiel R.
Remapping of Greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections
author_facet Goelzer, Heiko
Noël, Brice P. Y.
Edwards, Tamsin L.
Fettweis, Xavier
Gregory, Jonathan M.
Lipscomb, William H.
Wal, Roderik S. W.
Broeke, Michiel R.
author_sort Goelzer, Heiko
title Remapping of Greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections
title_short Remapping of Greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections
title_full Remapping of Greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections
title_fullStr Remapping of Greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections
title_full_unstemmed Remapping of Greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections
title_sort remapping of greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections
publishDate 2020
url https://doi.org/10.5194/tc-14-1747-2020
https://tc.copernicus.org/articles/14/1747/2020/
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-14-1747-2020
https://tc.copernicus.org/articles/14/1747/2020/
op_doi https://doi.org/10.5194/tc-14-1747-2020
container_title The Cryosphere
container_volume 14
container_issue 6
container_start_page 1747
op_container_end_page 1762
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