Modelled Antarctic firn depth averaged over 1979-2013 and corresponding brine zones area

The firn densification model IMAU-FDM has been used to simulate the firn density profile around Antarctica. The model is forced at the surface with climate data from the RACMO2.3 regional climate model. Here we provide the depth of three key firn density layers below the surface (750, 800 and 830 kgm^-3), averaged over the period 1979-2013. The data is on a horizontal grid of 27x27 km. The depth of each of these density layers was then subtracted from the surface elevation provided by Bedmap2 to determine where permeable firn exists below sea level. This defines the "brine zone" - the region where seawater may infiltrate the firn layer. We also provide shapefiles mapping the brine zone for each of three stated densities.

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Cite this as

Cook, Sue, Galton-Fenzi, Ben, Ligtenberg, Stefan R M, Wiltshire, Karen Helen (2018). Dataset: Modelled Antarctic firn depth averaged over 1979-2013 and corresponding brine zones area. https://doi.org/10.1594/PANGAEA.896384

DOI retrieved: 2018

Additional Info

Field Value
Imported on November 30, 2024
Last update November 30, 2024
License CC-BY-4.0
Source https://doi.org/10.1594/PANGAEA.896384
Author Cook, Sue
Given Name Sue
Family Name Cook
More Authors
Galton-Fenzi, Ben
Ligtenberg, Stefan R M
Wiltshire, Karen Helen
Source Creation 2018
Publication Year 2018
Subject Areas
Name: Ecology

Related Identifiers
Title: Brief communication: widespread potential for seawater infiltration on Antarctic ice shelves
Identifier: https://doi.org/10.5194/tc-12-3853-2018
Type: DOI
Relation: IsSupplementTo
Year: 2018
Source: The Cryosphere
Authors: Cook Sue , Galton-Fenzi Ben , Ligtenberg Stefan R M , Coleman Richard .