Preprints
https://doi.org/10.5194/egusphere-2024-2880
https://doi.org/10.5194/egusphere-2024-2880
23 Oct 2024
 | 23 Oct 2024
Status: this preprint is open for discussion.

Groundwater dynamics beneath a marine ice sheet

Gabriel Cairns, Graham Benham, and Ian Hewitt

Abstract. Sedimentary basins beneath many Antarctic ice streams host substantial volumes of groundwater, which can be exchanged with a “shallow” subglacial hydrological system of till and channelised water. This exchange contributes substantially to basal water budgets, which in turn modulate the flow of ice streams. The geometry of these sedimentary basins is known to be complex, and the groundwater therein has been observed to vary in salinity due to historic seawater intrusion. However, little is known about the hydraulic properties of subglacial sedimentary basins, and the factors controlling groundwater exfiltration and infiltration. We develop a mathematical model for two-dimensional groundwater flow beneath a marine-terminating ice stream on geological timescales, taking into account the effect of seawater intrusion. We find that seawater may become “trapped” in subglacial sedimentary basins, through cycles of grounding line advance and retreat or through “pockets” arising from basin geometry. In addition, we estimate the sedimentary basin permeability which reproduces field observations of groundwater salinity profiles from beneath Whillans Ice Stream in West Antarctica. Exchange of groundwater with the shallow hydrological system is primarily controlled by basin geometry, with groundwater being exfiltrated where the basin becomes shallower and re-infiltrating where it becomes deeper. However, seawater intrusion also has non-negligible effects on this exchange.

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Gabriel Cairns, Graham Benham, and Ian Hewitt

Status: open (until 04 Dec 2024)

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Gabriel Cairns, Graham Benham, and Ian Hewitt

Model code and software

Groundwater dynamics beneath a marine ice sheet – code Gabriel Cairns https://doi.org/10.5281/zenodo.13759411

Video supplement

Groundwater dynamics beneath a marine ice sheet – supplementary animations Gabriel Cairns https://doi.org/10.5281/zenodo.13759494

Gabriel Cairns, Graham Benham, and Ian Hewitt

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Short summary
Thick layers of porous rock known as sedimentary basins lie underneath many glaciers in Antarctica that flow into the sea. These layers contain large amounts of groundwater, some of which is seawater. We use a mathematical model to predict how groundwater flows through these basins, finding that seawater can become trapped due to changes in the ice sheet over time. We also predict where water flows out of (or into) these basins, and we discuss possible implications for the glacier.