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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 1
The Cryosphere, 9, 385-398, 2015
https://doi.org/10.5194/tc-9-385-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 9, 385-398, 2015
https://doi.org/10.5194/tc-9-385-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 20 Feb 2015

Research article | 20 Feb 2015

Seismic wave propagation in anisotropic ice – Part 2: Effects of crystal anisotropy in geophysical data

A. Diez1,2,*, O. Eisen1,3, C. Hofstede1, A. Lambrecht4, C. Mayer4, H. Miller1, D. Steinhage1, T. Binder5,**, and I. Weikusat1,6 A. Diez et al.
  • 1Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany
  • 2Karlsruhe Institute of Technology, Karlsruhe, Germany
  • 3Department Geosciences, University of Bremen, Bremen, Germany
  • 4Bavarian Academy for Sciences and Humanities, Munich, Germany
  • 5Interdisciplinary Center for Scientific Computing, University of Heidelberg, Heidelberg, Germany
  • 6Department of Geosciences, Eberhard Karls University of Tübingen, Tübingen, Germany
  • *now at: Scripps Institution of Oceanography, University of California, San Diego, USA
  • **now at: Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany

Abstract. We investigate the propagation of seismic waves in anisotropic ice. Two effects are important: (i) sudden changes in crystal orientation fabric (COF) lead to englacial reflections; (ii) the anisotropic fabric induces an angle dependency on the seismic velocities and, thus, recorded travel times. Velocities calculated from the polycrystal elasticity tensor derived for the anisotropic fabric from measured COF eigenvalues of the EDML ice core, Antarctica, show good agreement with the velocity trend determined from vertical seismic profiling. The agreement of the absolute velocity values, however, depends on the choice of the monocrystal elasticity tensor used for the calculation of the polycrystal properties. We make use of abrupt changes in COF as a common reflection mechanism for seismic and radar data below the firn–ice transition to determine COF-induced reflections in either data set by joint comparison with ice-core data. Our results highlight the possibility to complement regional radar surveys with local, surface-based seismic experiments to separate isochrones in radar data from other mechanisms. This is important for the reconnaissance of future ice-core drill sites, where accurate isochrone (i.e. non-COF) layer integrity allows for synchronization with other cores, as well as studies of ice dynamics considering non-homogeneous ice viscosity from preferred crystal orientations.

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