Award Abstract # 0440847
Detection of Crystal Orientation Fabrics near the Ross/Amundsen Sea Ice-flow Divide and at the Siple Dome Ice Core Site using Polarimetric Radar Methods

NSF Org: OPP
Office of Polar Programs (OPP)
Recipient: UNIVERSITY OF WASHINGTON
Initial Amendment Date: June 6, 2005
Latest Amendment Date: April 29, 2010
Award Number: 0440847
Award Instrument: Standard Grant
Program Manager: Julie Palais
OPP
 Office of Polar Programs (OPP)
GEO
 Directorate for Geosciences
Start Date: June 15, 2005
End Date: May 31, 2011 (Estimated)
Total Intended Award Amount: $0.00
Total Awarded Amount to Date: $442,908.00
Funds Obligated to Date: FY 2005 = $442,908.00
History of Investigator:
  • Charles Raymond (Principal Investigator)
    charlie@geophys.washington.edu
  • Kenichi Matsuoka (Co-Principal Investigator)
Recipient Sponsored Research Office: University of Washington
4333 BROOKLYN AVE NE
SEATTLE
WA  US  98195-1016
(206)543-4043
Sponsor Congressional District: 07
Primary Place of Performance: University of Washington
4333 BROOKLYN AVE NE
SEATTLE
WA  US  98195-1016
Primary Place of Performance
Congressional District:
07
Unique Entity Identifier (UEI): HD1WMN6945W6
Parent UEI:
NSF Program(s): ANT Glaciology
Primary Program Source: 0100CYXXDB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, OTHR
Program Element Code(s): 511600
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.078

ABSTRACT

This award supports a project to investigate fabrics with ground-based radar measurements near the Ross/Amundsen Sea ice-flow divide where a deep ice core will be drilled. The alignment of crystals in ice (crystal-orientation fabric) has an important effect on ice deformation. As ice deforms, anisotropic fabrics are produced, which, in turn, influence further deformation. Measurement of ice fabric variations can help reveal the deformation history of the ice and indicate how the ice will deform in the future. Ice cores provide opportunities to determine a vertical fabric profile, but horizontal variations of fabrics remain unknown. Remote sensing with ice-penetrating radar is the only way to do that over large areas. Preliminary results show that well-established polarimetric methods can detect the degree of horizontal anisotropy of fabrics and their orientation, even when they are nearly vertical-symmetric fabrics. In conjunction with ice deformation history, our first mapping of ice fabrics will contribute to modeling ice flow near the future ice core site. The project will train a graduate student and provide research experiences for two under graduate students both in field and laboratory. The project will contribute to ongoing West Antarctic ice sheet program efforts to better understand the impact of the ice sheet on global sea level rise. This project also supports an international collaboration between US and Japanese scientists.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Conway, Smith, Vaswani, Matsuoka, Rignot and Claus "A low-frequency ice-penetrating radar system adapted for use from an airplane: test results from Bering and Malaspina Glaciers, Alaska, USA" Annals of Glaciology , v.50 , 2009 , p.93
Fujita, S., H. Maeno and K. Matsuoka "Radio wave depolarization and scattering within ice sheets: A matrix based model to link radar and ice core measurements and its application" Journal of Glaciology , v.52 , 2006 , p.407
Matsuoka, Wilen, Shawn, and Raymond "Effects of birefringence within ice sheets on Obliquely Propagating Radio Wave" IEEE Trans Geoscience and Remote Sensing , v.47 , 2009 , p.1429 10.1109/TGRS.2008.2005201
Matsuoka, Wilen, Shawn, and Raymond "Effects of birefringence within ice sheets on Obliquely Propagating Radio Waves" IEEE Trans Geoscience and Remote Sensing , v.47 , 2009 , p.1429 10.1109/TGRS.2008.2005201

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