ATTENTION: The software behind KU ScholarWorks is going to be upgraded to a new version toward the end of July. Starting July 15th, users will not be able to log in to the system until the new version is in place. Searching for articles and opening files will continue to work while the system is being updated. If you have any questions, please contact Marianne Reed at mreed@ku.edu .

Show simple item record

dc.contributor.authorAllen, Christopher Thomas
dc.contributor.authorGogineni, Sivaprasad
dc.contributor.authorPaden, John D.
dc.contributor.authorJezek, Kenneth C.
dc.contributor.authorDahl-Jensen, Dorthe
dc.contributor.authorLarsen, Lars B.
dc.date.accessioned2007-04-04T21:23:09Z
dc.date.available2007-04-04T21:23:09Z
dc.date.issued2005-04
dc.identifier.citationPaden, JD; Allen, CT; Gogineni, S; Jezek, KC; Dahl-Jensen, D; Larsen, LB. Wideband measurements of ice sheet attenuation and basal scattering. IEEE GEOSCIENCE AND REMOTE SENSING LETTERS. April 2005. 2(2) : 164-168
dc.identifier.urihttp://hdl.handle.net/1808/1273
dc.description©2005 IEEE. Personal use of this material is permitted. However, permission to reprint/republish this material for advertising or promotional purposes or for creating new collective works for resale or redistribution to servers or lists, or to reuse any copyrighted component of this work in other works must be obtained from the IEEE.
dc.description.abstractWe are developing a multifirequency multistatic synthetic aperture radar (SAR) for determining polar ice sheet basal conditions. To obtain data for designing and optimizing radar performance, we performed field measurements with a network-analyzer-based system during the 2003 field season at the North Greenland Ice Core Project camp (75.1 N and 42.3 W). From the measurements, we determine the ice sheet complex transfer function over the frequency range from 110-500 MHz by deconvolving out the system transfer function. Over this frequency range, we observe an increase in total loss of 8 +/- 2.5 dB using a linear regression to the log-scale data. With the ice sheet transfer function and an ice extinction model, we estimate the return loss from the basal surface to be approximately 37 dB. These measurements have broad applicability to interpreting radar-sounding data, which are widely used in glaciological studies of the polar ice sheets. These data have also been used in the link budget for the design considerations of the multifirequency multistatic SAR system.
dc.language.isoen_US
dc.publisherIEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
dc.subjectIce
dc.subjectUltrahigh frequency measurements
dc.subjectVery high frequency measurements
dc.titleWideband measurements of ice sheet attenuation and basal scattering
dc.typeArticle
dc.identifier.doi10.1109/LGRS.2004.842474
dc.identifier.orcidhttps://orcid.org/0000-0002-1474-1948
dc.rights.accessrightsopenAccess


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record