Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/9323
Title: The effects of conductivity on high-resolution impulse radar sounding, Ross Ice Shelf, Antarctica
Authors: National Science Foundation (U.S.). Division of Polar Programs
Morey, Rexford M.
Kovacs, Austin
Keywords: Antarctica
Cold regions
Electrical conductivity
Ice
Sea Ice
Ice shelves
Ice thickness
Polar regions
Radar
Radar reconnaissance
EPOLAR
Publisher: Cold Regions Research and Engineering Laboratory (U.S.)
Engineer Research and Development Center (U.S.)
Series/Report no.: CRREL report ; 82-42.
Description: CRREL Report
Abstract: A high-resolution impulse radar profiling system was evaluated for 1.) detecting the presence of sea ice which coring has revealed to exist on the bottom of the Ross Ice Shelf at Site J -9, 2.) detecting the preferred horizontal c-axis azimuthal direction of the sea ice crystals, using the voltage amplitude of the radar reflection from the sea ice bottom, and 3.) determining the direction of the currents under an Antarctic ice shelf. A field program was conducted consisting of a surface radar survey on the Ross Ice Shelf at Site J-9 and surface and airborne radar profiling on the McMurdo Ice Shelf. The CRREL impulse radar system, operating at a center frequency of either 80 MHz or 20 MHz, was unable to detect the shelf bottom at Site J-9, which drilling revealed to be 416 m below the snow surface. The radar system was used to profile the McMurdo Ice Shelf both from the snow surface and from the air; a shelf thickness of about 275 m was easily detected. Theoretical considerations indicate that the bulk conductivity of the ice shelf at Site J·9 was higher than originally anticipated, and this limited the radar sounding depth to about 405 m when operating at a frequency of 20 MHz.
Rights: Approved for public release; distribution is unlimited.
URI: http://hdl.handle.net/11681/9323
Appears in Collections:CRREL Report

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