Radar sounding is a powerful geophysical approach for characterizing the subsurface
conditions of terrestrial and planetary ice masses at local to global scales. As a result, a wide …

Abstract The Radar for Europa Assessment and Sounding: Ocean to Near-surface
(REASON) is a dual-frequency ice-penetrating radar (9 and 60 MHz) onboard the Europa …

Antarctic subglacial lakes are studied for three main scientific reasons. First, they form an
important component of the basal hydrological system which is known to affect the dynamics …

Thwaites Glacier is one of the largest, most rapidly changing glaciers on Earth, and its
landward-slo** bed reaches the interior of the marine West Antarctic Ice Sheet, which …

Abstract Knowledge of Antarctica's sedimentary basins builds our understanding of the
coupled evolution of tectonics, ice, ocean, and climate. Sedimentary basins have properties …

Heterogeneous hydrologic, lithologic, and geologic basal boundary conditions can exert
strong control on the evolution, stability, and sea level contribution of marine ice sheets …

The flow of ice is temperature‐dependent, but direct measurements of englacial temperature
are sparse. The dielectric attenuation of radio waves through ice is also temperature …

Antarctic subglacial lakes can play an important role in ice sheet dynamics, biology,
geology, and oceanography, but it is difficult to definitively constrain their character and …

Surface meltwater that reaches the base of the Greenland Ice Sheet exerts a fundamental
impact on ice flow, but observations of catchment‐wide movement and distribution of …

To better understand the ability of ice-penetrating radar to diagnose the subglacial
environment from bed-returned power, we model the englacial radar attenuation of Antarctic …