Hydrologic properties of a highly permeable firn aquifer in the Wilkins Ice Shelf, Antarctica

We present measurements of the density, hydraulic conductivity, and specific discharge of a widespread firn aquifer in Antarctica, within the Wilkins Ice Shelf. At the field site, the aquifer is 16.2 m thick, starting at 13.4 m from the snow surface and transitioning from water‐saturated firn to ice at 29.6 m. Hydraulic conductivity derived from slug tests show a geometric mean value of 1.4 ± 1.2 × 10⁻⁴ m s⁻¹, equivalent to permeability of 2.6 ± 2.2 × 10⁻¹¹ m². A borehole dilution test indicates an average specific discharge value of 1.9 ± 2.8 × 10⁻⁶ m s⁻¹. Ground‐penetrating radar profiles and a groundwater flow model show the aquifer is draining laterally into a large nearby rift. Our findings indicate that the firn aquifer in the vicinity of the field site is likely not in a steady state and its presence likely contributed to past ice shelf instability.