Antarctica is host to a volume of ice equivalent to 57.9 Β± 0.9 m of global mean sea level (GMSL) rise, or roughly 90% of the global cryosphere (Bamber et al., 2018;Morlighem et al., 2020). The mantle structure, topography, and glacial stability of this continent expresses a dichotomy in tectonic setting between East and West Antarctica. The two regions are separated by the Transantarctic Mountain Range (TAM), which spans the continental interior from the Weddell Sea (WS) to the Ross Sea (RS). As a result, Antarctica's grounded ice volume is divided into an East and West Antarctic Ice Sheet (EAIS and WAIS, respectively). The EAIS is underlain by thick, cratonic lithosphere owing to minimal tectonic activity in this region since the Mesozoic Era (Noble et al., 2020). The WAIS is underlain by an active rift system, which has given rise to upwelling of low viscosity asthenosphere, and dynamically thinned lithosphere (Noble et al., 2020). Bedrock elevation is predominantly above GMSL in