Journal cover Journal topic
The Cryosphere An interactive open-access journal of the European Geosciences Union
The Cryosphere, 9, 385-398, 2015
http://www.the-cryosphere.net/9/385/2015/
doi: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
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 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.

Citation: Diez, A., Eisen, O., Hofstede, C., Lambrecht, A., Mayer, C., Miller, H., Steinhage, D., Binder, T., and Weikusat, I.: Seismic wave propagation in anisotropic ice – Part 2: Effects of crystal anisotropy in geophysical data, The Cryosphere, 9, 385-398, doi:10.5194/tc-9-385-2015, 2015.
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