TC - Seismic attenuation in Antarctic firn
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
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Measuring seismic attenuation in polar firn: method and application to Korff Ice Rise, West Antarctica, Journal of Glaciology
Frontiers West Antarctic Ice Sheet Dynamics in the Amundsen Sea Sector since the Late Miocene—Tying IODP Expedition 379 Results to Seismic Data
Measuring seismic attenuation in polar firn: method and application to Korff Ice Rise, West Antarctica, Journal of Glaciology
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PDF) Seismic attenuation in Antarctic firn
Spatial variation of englacial radar attenuation: Modeling
Remote Sensing, Free Full-Text
Frontiers West Antarctic Ice Sheet Dynamics in the Amundsen Sea Sector since the Late Miocene—Tying IODP Expedition 379 Results to Seismic Data
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