Moulin density controls drainage development beneath the Greenland ice sheet
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Peer-reviewed
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Abstract
Uncertainty remains about how the surface hydrology of the Greenland ice sheet influences its subglacial drainage system, affecting basal water pressures and ice velocities, particularly over intraseasonal and interseasonal timescales. Here we apply a high spatial (200m) and temporal (1h) resolution subglacial hydrological model to a marginal (extending ~25km inland), land-terminating, ~200km
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2169-9011
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Isaac Newton Trust (1408(g))