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Hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages

Ching-Yao Lai (), Laura A. Stevens, Danielle L. Chase, Timothy T. Creyts, Mark D. Behn, Sarah B. Das and Howard A. Stone
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Ching-Yao Lai: Princeton University
Laura A. Stevens: Columbia University
Danielle L. Chase: Princeton University
Timothy T. Creyts: Columbia University
Mark D. Behn: Boston College
Sarah B. Das: Woods Hole Oceanographic Institution
Howard A. Stone: Princeton University

Nature Communications, 2021, vol. 12, issue 1, 1-10

Abstract: Abstract Surface meltwater reaching the base of the Greenland Ice Sheet transits through drainage networks, modulating the flow of the ice sheet. Dye and gas-tracing studies conducted in the western margin sector of the ice sheet have directly observed drainage efficiency to evolve seasonally along the drainage pathway. However, the local evolution of drainage systems further inland, where ice thicknesses exceed 1000 m, remains largely unknown. Here, we infer drainage system transmissivity based on surface uplift relaxation following rapid lake drainage events. Combining field observations of five lake drainage events with a mathematical model and laboratory experiments, we show that the surface uplift decreases exponentially with time, as the water in the blister formed beneath the drained lake permeates through the subglacial drainage system. This deflation obeys a universal relaxation law with a timescale that reveals hydraulic transmissivity and indicates a two-order-of-magnitude increase in subglacial transmissivity (from 0.8 ± 0.3 $${\rm{m}}{{\rm{m}}}^{3}$$ m m 3 to 215 ± 90.2 $${\rm{m}}{{\rm{m}}}^{3}$$ m m 3 ) as the melt season progresses, suggesting significant changes in basal hydrology beneath the lakes driven by seasonal meltwater input.

Date: 2021
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DOI: 10.1038/s41467-021-24186-6

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