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 Vol. 12; no. 5; pp. 1643 - 1649 |
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Main Authors | , , , |
Format | Journal Article Web Resource |
Language | English |
Published |
Katlenburg-Lindau
Copernicus GmbH
08.05.2018
Copernicus Publications |
Subjects | |
Online Access | Get full text |
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Summary: | 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. |
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Bibliography: | scopus-id:2-s2.0-85046875184 |
ISSN: | 1994-0424 1994-0416 1994-0424 1994-0416 |
DOI: | 10.5194/tc-12-1643-2018 |