HR: 1340h
AN: T13B-1335 [Abstracts]
TI: Effects of birefringence within ice sheets on bistatic radar measurements
AU: * Matsuoka, K
EM: matsuoka@ess.washington.edu
AF: Department of Earth and Space Sciences, University of Washington, Box 351310, Seattle,
WA 98195, United States
AU: Wilen, L
EM: wilen@helios.phy.ohiou.edu
AF: Department of Physics and Astronomy, Ohio University, Clippinger Lab 251B, Athens, CO
45701, United States
AU: Hurley, S P
EM: shurley@lci.kent.edu
AF: Department of Physics and Astronomy, Ohio University, Clippinger Lab 251B, Athens, CO
45701, United States
AU: Raymond, C F
EM: cfr@ess.washington.edu
AF: Department of Earth and Space Sciences, University of Washington, Box 351310, Seattle,
WA 98195, United States
AB:
Ice fabric is known to affect radio wave propagation within polar ice sheets. Strong vertical contrasts in the fabric
cause reflection, while anisotropy in the fabric integrated along the propagation path causes birefringence.
Bistatic radar measurements (i.e. using a transmitter and receiver separated from each other) have more
potential to assess fabric than monostatic measurements, because they allow more general geometric
relationships between the radio wave and ice fabric. We worked out the effect of fabric on radio waves
propagating obliquely through the polar ice sheets in terms of radar frequency, polarization and geometry of the
propagation path. The model is applied to fabrics that approximate those found in the polar ice sheets. When ice
fabrics are unknown, the geometry of the propagation path relative to the ice fabric is arbitrary. In this case, 1-km-
thick ice with a quite gentle and strongly developed fabric causes significant (> 1 dB) birefringence-origin echo
variations at radar frequencies higher than 200 MHz and 20 MHz, respectively. An azimuthal pattern of the echo
collected with bistatic radar is 90° periodic, not 45° as found in the vertical propagation (monostatic radar
sounding). It suggests that bistatic radar can be used to identify principal axes of the ice fabric.
DE: 0776 Glaciology (1621, 1827, 1863)
DE: 6964 Radio wave propagation
DE: 6994 Instruments and techniques (1241)
SC: Tectonophysics [T]
MN: 2007 Fall Meeting