Constraining recent ice flow history at Korff Ice Rise, West Antarctica, using radar and seismic measurements of ice fabric

Brisbourne, Alex M. ORCID: https://orcid.org/0000-0002-9887-7120; Martin, Carlos ORCID: https://orcid.org/0000-0002-2661-169X; Smith, Andy M. ORCID: https://orcid.org/0000-0001-8577-482X; Baird, A.F.; Kendall, J.M.; Kingslake, J.. 2019 Constraining recent ice flow history at Korff Ice Rise, West Antarctica, using radar and seismic measurements of ice fabric. Journal of Geophysical Research: Earth Surface, 124 (1). 175-194. 10.1029/2018JF004776

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Text ©2019. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. Brisbourne_et_al-2019-Journal_of_Geophysical_Research__Earth_Surface.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (3MB) | Preview

Abstract/Summary

The crystal orientation fabric of ice reflects its flow history, information which is required to better constrain projections of future ice sheet behavior. Here we present a novel combination of polarimetric phase‐sensitive radar and seismic anisotropy measurements to provide independent and consistent constraints on ice fabric at Korff Ice Rise, within the Weddell Sea sector of West Antarctica. The nature and depth distribution of fabric in the ice column is constrained using the azimuthal variation in (1) the received power anomaly and phase difference of polarimetric vertical radar soundings and (2) seismic velocities and shear wave splitting measurements. Radar and seismic observations are modeled separately to determine the nature and strength of fabric within the ice column. Both methods indicate ice fabric above 200‐m depth which is consistent with present‐day ice‐divide flow. However, both measurements also indicate an oblique girdle fabric below 230‐m depth within the ice column, inconsistent with steady state divide flow. Our interpretation is that this deeper fabric is a remnant fabric from a previous episode of flow, which is currently being overwritten by ongoing fabric development associated with the present‐day flow regime. The preexisting fabric is consistent with ice flow from the south prior to ice‐divide formation, in agreement with models of Holocene ice sheet evolution. These findings apply new constraints to the flow history at Korff Ice Rise prior to divide formation and demonstrate the capacity of radar and seismic measurements to map fabric and thus constrain past ice flow.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1029/2018JF004776
Additional Keywords:	Antarctica anisotropy fabric ice sheet history seismic Antarctica, anisotropy, fabric, ice sheet history, seismic, radar
Date made live:	19 Mar 2019 14:06 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/520190

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