TC - Seismic attenuation in Antarctic firn
By A Mystery Man Writer
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
Frontiers Tidal Modulation of a Lateral Shear Margin: Priestley Glacier, Antarctica
Seismo-Geophysical Studies in the Antarctic Region: Geodynamical Implications
Basal conditions at the grounding zone of Whillans Ice Stream
Geosciences, Free Full-Text
Geosciences, Free Full-Text
Enhanced Firn Densification in High‐Accumulation Shear Margins of
Ambient high-frequency seismic surface waves in the firn column of
Measuring seismic attenuation in polar firn: method and application to Korff Ice Rise, West Antarctica, Journal of Glaciology
TC - Seismic attenuation in Antarctic firn
- CRZ YOGA Women's Yoga High Rise Air Feeling Yoga Leggings 28
- Effect of air inlet and outlet cross sections on the cooling
- Two-dimensional metal-organic frameworks: From synthesis to biomedical, environmental, and energy conversion applications - ScienceDirect
- Post-lithium-ion battery cell production and its compatibility with lithium-ion cell production infrastructure
- Enabling 4.6 V LiNi0.6Co0.2Mn0.2O2 cathodes with excellent structural stability: combining surface LiLaO2 self-assembly and subsurface La-pillar engineering
