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Record #112070:

Dielectric permittivity and scattering loss measurements of Greenland firn at Ka-band / V.I. Lytle, Kenneth C. Jezek.

Title: Dielectric permittivity and scattering loss measurements of Greenland firn at Ka-band / V.I. Lytle, Kenneth C. Jezek.
Author(s): Lytle, V. I.
Jezek, Kenneth C.
Date: 1991.
In: Eos : transactions, American Geophysical Union. (1991.), Vol. 72(44, supplement) (1991)
Abstract: AGU Fall Meeting Program and Abstracts, December 9-13, 1991. Measured dielectric permittivity varied from 1.7 to 1.9, and was found to be anisotropic, with an increased permittivity in two firn samples when electric field was oriented perpendicular to firn layers. Analysis of firn indicated that grains were elongated in this same direction. Transmission losses varied, with average at 3 dB m⁻¹ through firn when using full radar bandwidth. Using only higher portion of bandwidth (33.5 to 40.0 GHz), losses were about 5 dB m⁻¹.
Notes:

Eos : transactions, American Geophysical Union. Vol. 72(44, supplement) :150 (1991).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.24 -- Ice sheets and caps.
53.087.23 -- Remote sensing.
621.396.96 -- Radar.
537.226 -- Ice, dielectrical properties.
534.2 -- Acoustics in ice.
548 -- Crystallography.
E5 -- Glaciology: land ice.
(*38) -- Greenland.
SPRI record no.: 112070

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100 1# ‡aLytle, V. I.
245 10 ‡aDielectric permittivity and scattering loss measurements of Greenland firn at Ka-band /‡cV.I. Lytle, Kenneth C. Jezek.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 150.
500 ## ‡aEos : transactions, American Geophysical Union. Vol. 72(44, supplement) :150 (1991).
520 3# ‡aAGU Fall Meeting Program and Abstracts, December 9-13, 1991. Measured dielectric permittivity varied from 1.7 to 1.9, and was found to be anisotropic, with an increased permittivity in two firn samples when electric field was oriented perpendicular to firn layers. Analysis of firn indicated that grains were elongated in this same direction. Transmission losses varied, with average at 3 dB m⁻¹ through firn when using full radar bandwidth. Using only higher portion of bandwidth (33.5 to 40.0 GHz), losses were about 5 dB m⁻¹.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc
650 07 ‡a53.087.23 -- Remote sensing.‡2udc
650 07 ‡a621.396.96 -- Radar.‡2udc
650 07 ‡a537.226 -- Ice, dielectrical properties.‡2udc
650 07 ‡a534.2 -- Acoustics in ice.‡2udc
650 07 ‡a548 -- Crystallography.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*38) -- Greenland.‡2udc
700 1# ‡aJezek, Kenneth C.
773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 72(44, supplement) (1991) ‡wSPRI-1028
917 ## ‡aUnenhanced record from Muscat, imported 2019
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