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Record #152538:
- #152538
Main publication details
MARC recordVelocity 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 |
LDR 01606naa#a2200000#a#4500 001 SPRI-152538 005 20231211033632.0 007 ta 008 231211s1999####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-152538 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aLiu, C. 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 948 3# ‡a20231211