Adaptively constraining radar attenuation and temperature across the Thwaites Glacier catchment using bed echoes

Englacial temperature is a major control on ice rheology and flow.However, it is difficult to measure at the glacier to ice-sheet scale.As a result, ice-sheet models must make assumptions about englacial temperature and rheology, which affect sea level projections.This is problematic if fundamental processes are not captured by models due to a lack

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