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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Seismic observations of a complex firn structure across the Amery Ice Shelf, East Antarctica, Journal of Glaciology
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TC - Seismic attenuation in Antarctic firn
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Frontiers West Antarctic Ice Sheet Dynamics in the Amundsen Sea Sector since the Late Miocene—Tying IODP Expedition 379 Results to Seismic Data
Location map showing the seismic profiles (lines 1-4) crossing the
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Remote Sensing, Free Full-Text
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Frontiers West Antarctic Ice Sheet Dynamics in the Amundsen Sea Sector since the Late Miocene—Tying IODP Expedition 379 Results to Seismic Data
![TC - Seismic attenuation in Antarctic firn](https://library.seg.org/cms/10.1190/geo2015-0122.1/asset/images/medium/figure9.gif)
Evidence for variable grounding-zone and shear-margin basal
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TC - Relations - Seismic attenuation in Antarctic firn
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Abstract Booklet - isaes 2011
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