Abstract. We estimate the seismic attenuation of P and S waves in the polar firn and underlying ice by spectral analysis of diving, refracted, and reflected waves from active-source three-component seismic signals obtained in 2010 on the Whillans Ice Stream (WIS), a fast-flowing ice stream in West Antarctica. The resulting quality factors are then successfully modeled using a rock-physics theory of wave propagation that combines White
Antarctic supraglacial lakes and ice-shelf collapse
Predicting radar attenuation within the Antarctic ice sheet - ScienceDirect
Predicting radar attenuation within the Antarctic ice sheet - ScienceDirect
TC - Seismic attenuation in Antarctic firn
Frontiers Investigation of Firn Aquifer Structure in
TC - Seismic attenuation in Antarctic firn
TC - Relations - Seismic attenuation in Antarctic firn
Spatial variation of englacial radar attenuation: Modeling
Predicting radar attenuation within the Antarctic ice sheet - ScienceDirect
Calculating glacier ice volumes and sea level equivalents
Missing Evidence of Widespread Subglacial Lakes at Recovery Glacier, Antarctica - Humbert - 2018 - Journal of Geophysical Research: Earth Surface - Wiley Online Library
The marine geological imprint of Antarctic ice shelves
Measuring seismic attenuation in polar firn: method and application to Korff Ice Rise, West Antarctica, Journal of Glaciology
The 80 MPH Glacier Fracture: A Wake-Up Call From Antarctica
