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Abstract

Ground-penetrating radar data acquired in the 2016/17 austral summer on Sørsdal Glacier, East Antarctica, provide evidence for meltwater lenses within porous surface ice that are conceptually similar to firn aquifers observed on the Greenland Ice Sheet and the Arctic and Alpine glaciers. These englacial water bodies are associated with a dry relict surface basin and consistent with perennial drainage into an interconnected englacial drainage system, which may explain a large englacial outburst flood observed in satellite imagery in the early 2016/17 melt season. Our observations indicate the rarely-documented presence of an englacial hydrological system in Antarctica, with implications for the storage and routing of surface meltwater. Future work should ascertain the spatial prevalence of such systems around the Antarctic coastline, and identify the degree of surface runoff redistribution and storage in the near surface, to quantify their impact on surface mass balance.

Item Type:	Article
Authors/Creators:	Schaap, T and Roach, MJ and Peters, LE and Cook, S and Kulessa, B and Schoof, C
Keywords:	Antarctica, glacier geophysics, glacier hydrology, ground-penetrating radar
Journal or Publication Title:	Journal of Glaciology
Publisher:	Int Glaciol Soc
ISSN:	0022-1430
DOI / ID Number:	10.1017/ jog.2019.92
Copyright Information:	Copyright 2019 The Authors. Licensed under Creative Commons Attribution 4.0 International (CC BY 4.0) https://creativecommons.org/licenses/by/4.0/
Related URLs:	UTAS Profile: Roach, MJ Google Scholar: Cook, S UTAS Profile: Cook, S
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