Anisotropy and crystalline fabric of whillans ice stream (West Antarctica) inferred frommulticomponent seismic data

Stefano Picotti, Alessandro Vuan, José M. Carcione, Huw J. Horgan, Sridhar Anandakrishnan

Research output: Contribution to journalArticle

19 Citations (Scopus)

Abstract

Crystal orientation fabric (COF) describes the intrinsic anisotropic nature of ice and is an important parameter for modeling glacier flow. We present the results of three-component active-source seismic observations from the Whillans Ice Stream (WIS), a fast-flowing ice stream in West Antarctica. Surface-wave dispersion analysis, ray tracing, and traveltime inversion of compressional (P) and shear (S) waves reveal the presence of transversely isotropic ice with a vertical axis of symmetry (VTI) beneath approximately 65 m of isotropic firn. The ice stream is characterized by weak anisotropy, involving an average ice thickness of approximately 780 m. The analysis indicates that about 95% of the ice mass is anisotropic, and the crystalline c axes span within an average broad cone angle of 73 ± 10° with respect to the vertical axis. Moreover, the mean temperature T (below the firn) estimated from seismic data is -15 ± 5°C. These data do not show evidence of englacial seismic reflectivity, which indicates the lack of abrupt changes in the COF. The presence of azimuthal anisotropy due to transversely compressive flow or fractures aligned along a preferential direction is also excluded. We suggest that the observed VTI ice structure is typical of large ice streams in regions where basal sliding and bed deformation dominate over internal glacial deformation.

Original languageEnglish (US)
Pages (from-to)4237-4262
Number of pages26
JournalJournal of Geophysical Research: Solid Earth
Volume120
Issue number6
DOIs
StatePublished - Jan 1 2015

Fingerprint

ice stream
Ice
Antarctic regions
seismic data
ice
Anisotropy
anisotropy
Crystalline materials
firn
S-wave
crystal
glacier flow
wave dispersion
seismic source
ice thickness
ray tracing
reflectivity
surface wave
sliding
symmetry

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

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title = "Anisotropy and crystalline fabric of whillans ice stream (West Antarctica) inferred frommulticomponent seismic data",
abstract = "Crystal orientation fabric (COF) describes the intrinsic anisotropic nature of ice and is an important parameter for modeling glacier flow. We present the results of three-component active-source seismic observations from the Whillans Ice Stream (WIS), a fast-flowing ice stream in West Antarctica. Surface-wave dispersion analysis, ray tracing, and traveltime inversion of compressional (P) and shear (S) waves reveal the presence of transversely isotropic ice with a vertical axis of symmetry (VTI) beneath approximately 65 m of isotropic firn. The ice stream is characterized by weak anisotropy, involving an average ice thickness of approximately 780 m. The analysis indicates that about 95{\%} of the ice mass is anisotropic, and the crystalline c axes span within an average broad cone angle of 73 ± 10° with respect to the vertical axis. Moreover, the mean temperature T (below the firn) estimated from seismic data is -15 ± 5°C. These data do not show evidence of englacial seismic reflectivity, which indicates the lack of abrupt changes in the COF. The presence of azimuthal anisotropy due to transversely compressive flow or fractures aligned along a preferential direction is also excluded. We suggest that the observed VTI ice structure is typical of large ice streams in regions where basal sliding and bed deformation dominate over internal glacial deformation.",
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Anisotropy and crystalline fabric of whillans ice stream (West Antarctica) inferred frommulticomponent seismic data. / Picotti, Stefano; Vuan, Alessandro; Carcione, José M.; Horgan, Huw J.; Anandakrishnan, Sridhar.

In: Journal of Geophysical Research: Solid Earth, Vol. 120, No. 6, 01.01.2015, p. 4237-4262.

Research output: Contribution to journalArticle

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