Seismic attenuation in Antarctic firn
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....
Published in: | The Cryosphere |
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Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
2024
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-18-169-2024 https://tc.copernicus.org/articles/18/169/2024/ |