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Record #152538:

Velocity difference between the surface and base of Ice Stream B2, West Antarctica, from radar fading-pattern experiment / C. Liu, Charles R. Bentley, N.E. Lord.

Title: Velocity difference between the surface and base of Ice Stream B2, West Antarctica, from radar fading-pattern experiment / C. Liu, Charles R. Bentley, N.E. Lord.
Author(s): Liu, C.
Bentley, Charles R.
Lord, N. E.
Date: 1999.
In: Annals of Glaciology. (1999.), Vol. 29 (1999)
Abstract: Describes spatial fading pattern obtained from ice-sounding radar receiver and transmitter moved together across surface of snow. Repeated measurements of fading pattern can reveal relative displacement between snow surface and targets near bed of ice and/or in ice. Three largest high-density grids (out of six) were significantly different. Differences may be related to complex systems of strains within ice stream reported previously.
Notes:

Annals of Glaciology. Vol. 29 :243-249 (1999).

Sixth International Symposium on Antarctic Glaciology (ISAG-6), 5--9 September 1998, Lanzhou, China, T.H. Jacka (Editor)

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.29 -- Land ice, miscellaneous forms: Ice Stream B2.
551.324.5 -- Land ice, flow.
621.396.96 -- Radar.
E5 -- Glaciology: land ice.
(*7) -- Antarctic regions.
(*7.7) -- West Antarctica.
SPRI record no.: 152538

MARCXML

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245 10 ‡aVelocity difference between the surface and base of Ice Stream B2, West Antarctica, from radar fading-pattern experiment /‡cC. Liu, Charles R. Bentley, N.E. Lord.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1999.
300 ## ‡ap. 243-249 :‡bill., diags., tables.
500 ## ‡aAnnals of Glaciology. Vol. 29 :243-249 (1999).
500 ## ‡aSixth International Symposium on Antarctic Glaciology (ISAG-6), 5--9 September 1998, Lanzhou, China, T.H. Jacka (Editor)
520 3# ‡aDescribes spatial fading pattern obtained from ice-sounding radar receiver and transmitter moved together across surface of snow. Repeated measurements of fading pattern can reveal relative displacement between snow surface and targets near bed of ice and/or in ice. Three largest high-density grids (out of six) were significantly different. Differences may be related to complex systems of strains within ice stream reported previously.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.29 -- Land ice, miscellaneous forms: Ice Stream B2.‡2udc
650 07 ‡a551.324.5 -- Land ice, flow.‡2udc
650 07 ‡a621.396.96 -- Radar.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*7.7) -- West Antarctica.‡2udc
700 1# ‡aBentley, Charles R.
700 1# ‡aLord, N. E.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 29 (1999) ‡wSPRI-60773
917 ## ‡aUnenhanced record from Muscat, imported 2019
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