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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Veröffentlicht in:The cryosphere 2020-06, Vol.14 (6), p.1747-1762
Hauptverfasser: Goelzer, Heiko, Noel, Brice P. Y., Edwards, Tamsin L., Fettweis, Xavier, Gregory, Jonathan M., Lipscomb, William H., van de Wal, Roderik S. W., van den Broeke, Michiel R.
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container_end_page 1762
container_issue 6
container_start_page 1747
container_title The cryosphere
container_volume 14
creator Goelzer, Heiko
Noel, Brice P. Y.
Edwards, Tamsin L.
Fettweis, Xavier
Gregory, Jonathan M.
Lipscomb, William H.
van de Wal, Roderik S. W.
van den Broeke, Michiel R.
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.
doi_str_mv 10.5194/tc-14-1747-2020
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subjects Ablation
Analysis
Anomalies
Basins
Climate
Climate change
Climate models
Drainage basins
Earth sciences & physical geography
Equilibrium
Geography, Physical
Geology
Geometry
Geosciences, Multidisciplinary
Glaciation
Greenland ice sheet
Ice
Ice sheet models
Ice sheets
Mass balance
Mass balance of ice sheets
Physical Geography
Physical Sciences
Physical, chemical, mathematical & earth Sciences
Physique, chimie, mathématiques & sciences de la terre
Prejudice
River basins
Science & Technology
Sciences de la terre & géographie physique
Sea level
Sea level anomalies
Sea level changes
Sheet modelling
Simulation
title Remapping of Greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections
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