TC - Seismic attenuation in Antarctic firn
By A Mystery Man Writer
Description
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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TC - Relations - Seismic attenuation in Antarctic firn
Map of Antarctica with the permanent seismic stations, and the seismic
a) Locations of firn surveys conducted at NEGIS around the EGRIP
TC - Seismic attenuation in Antarctic firn
PDF) Antarctic ice sheet thickness estimation using the horizontal
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PDF) Measuring seismic attenuation in polar firn: method and application to Korff Ice Rise, West Antarctica
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