title: Characterising Ice Slabs in Firn Using Seismic Full Waveform Inversion
abstract: The density structure of firn has implications for hydrological and climate modelling, and ice shelf stability. The structure of firn can be evaluated from depth models of seismic velocity, widely obtained with Herglotz-Wiechert Inversion (HWI), an approach that considers the slowness of refracted seismic arrivals. However, HWI is strictly appropriate only for steady-state firn profiles and the inversion accuracy can be compromised where firn contains ice layers. In these cases, Full Waveform In