Brief communication: Improved simulation of the present-day Greenland firn layer (1960–2016)

By providing pore space for storage or refreezing of meltwater, the Greenland ice sheet firn layer strongly modulates runoff. Correctly representing the firn layer is therefore crucial for Greenland (surface) mass balance studies. Here, we present a simulation of the Greenland firn layer with the fi...

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Published in:The Cryosphere
Main Authors: Ligtenberg, Stefan R. M., Kuipers Munneke, Peter, Noël, Brice P. Y., Broeke, Michiel R.
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/tc-12-1643-2018
https://tc.copernicus.org/articles/12/1643/2018/
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spelling ftcopernicus:oai:publications.copernicus.org:tc64965 2023-05-15T16:23:24+02:00 Brief communication: Improved simulation of the present-day Greenland firn layer (1960–2016) Ligtenberg, Stefan R. M. Kuipers Munneke, Peter Noël, Brice P. Y. Broeke, Michiel R. 2019-01-10 application/pdf https://doi.org/10.5194/tc-12-1643-2018 https://tc.copernicus.org/articles/12/1643/2018/ eng eng doi:10.5194/tc-12-1643-2018 https://tc.copernicus.org/articles/12/1643/2018/ eISSN: 1994-0424 Text 2019 ftcopernicus https://doi.org/10.5194/tc-12-1643-2018 2020-07-20T16:23:18Z By providing pore space for storage or refreezing of meltwater, the Greenland ice sheet firn layer strongly modulates runoff. Correctly representing the firn layer is therefore crucial for Greenland (surface) mass balance studies. Here, we present a simulation of the Greenland firn layer with the firn model IMAU-FDM forced by the latest output of the regional climate model RACMO2, version 2.3p2. In the percolation zone, much improved agreement is found with firn density and temperature observations. A full simulation of Greenland firn at high temporal (10 days) and spatial (11 km) resolution is available for the period 1960–2016. Text Greenland Ice Sheet Copernicus Publications: E-Journals Greenland The Cryosphere 12 5 1643 1649
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description By providing pore space for storage or refreezing of meltwater, the Greenland ice sheet firn layer strongly modulates runoff. Correctly representing the firn layer is therefore crucial for Greenland (surface) mass balance studies. Here, we present a simulation of the Greenland firn layer with the firn model IMAU-FDM forced by the latest output of the regional climate model RACMO2, version 2.3p2. In the percolation zone, much improved agreement is found with firn density and temperature observations. A full simulation of Greenland firn at high temporal (10 days) and spatial (11 km) resolution is available for the period 1960–2016.
format Text
author Ligtenberg, Stefan R. M.
Kuipers Munneke, Peter
Noël, Brice P. Y.
Broeke, Michiel R.
spellingShingle Ligtenberg, Stefan R. M.
Kuipers Munneke, Peter
Noël, Brice P. Y.
Broeke, Michiel R.
Brief communication: Improved simulation of the present-day Greenland firn layer (1960–2016)
author_facet Ligtenberg, Stefan R. M.
Kuipers Munneke, Peter
Noël, Brice P. Y.
Broeke, Michiel R.
author_sort Ligtenberg, Stefan R. M.
title Brief communication: Improved simulation of the present-day Greenland firn layer (1960–2016)
title_short Brief communication: Improved simulation of the present-day Greenland firn layer (1960–2016)
title_full Brief communication: Improved simulation of the present-day Greenland firn layer (1960–2016)
title_fullStr Brief communication: Improved simulation of the present-day Greenland firn layer (1960–2016)
title_full_unstemmed Brief communication: Improved simulation of the present-day Greenland firn layer (1960–2016)
title_sort brief communication: improved simulation of the present-day greenland firn layer (1960–2016)
publishDate 2019
url https://doi.org/10.5194/tc-12-1643-2018
https://tc.copernicus.org/articles/12/1643/2018/
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-12-1643-2018
https://tc.copernicus.org/articles/12/1643/2018/
op_doi https://doi.org/10.5194/tc-12-1643-2018
container_title The Cryosphere
container_volume 12
container_issue 5
container_start_page 1643
op_container_end_page 1649
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