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

Visualization of attenuation structure and faults in incoming oceanic crust of the Nankai Trough using seismic attenuation profiling, Earth, Planets and Space

Frontiers Investigation of Firn Aquifer Structure in

PDF) Measuring seismic attenuation in polar firn: method and application to Korff Ice Rise, West Antarctica

Predicting radar attenuation within the Antarctic ice sheet - ScienceDirect

PDF) Measuring seismic attenuation in polar firn: method and application to Korff Ice Rise, West Antarctica

PDF) Measuring seismic attenuation in polar firn: method and

Measuring seismic attenuation in polar firn: method and application to Korff Ice Rise, West Antarctica, Journal of Glaciology

The marine geological imprint of Antarctic ice shelves

IODP Publications • Volume 379 expedition reports • Expedition 379 summary