TC - Seismic attenuation in Antarctic firn
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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
Structures and Deformation in Glaciers and Ice Sheets - Jennings - 2021 - Reviews of Geophysics - Wiley Online Library
Elastic deformation plays a non-negligible role in Greenland's
TC - Relations - Seismic attenuation in Antarctic firn
Frontiers West Antarctic Ice Sheet Dynamics in the Amundsen Sea Sector since the Late Miocene—Tying IODP Expedition 379 Results to Seismic Data
The 80 MPH Glacier Fracture: A Wake-Up Call From Antarctica
TC - Seismic attenuation in Antarctic firn
Missing Evidence of Widespread Subglacial Lakes at Recovery Glacier, Antarctica - Humbert - 2018 - Journal of Geophysical Research: Earth Surface - Wiley Online Library
TC - Seismic attenuation in Antarctic firn
TC - Relations - Seismic attenuation in Antarctic firn
Ice Dynamics and Palaeoclimate team - British Antarctic Survey
TC - Relations - Seismic attenuation in Antarctic firn
