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Record #164646:
- #164646
Main publication details
MARC recordPost-stagnation behavior in the upstream regions of Ice Stream C, West Antarctica / S.F. Price, R.A. Bindschadler, C.L. Hulbe, I.R. Joughin.
| Title: | Post-stagnation behavior in the upstream regions of Ice Stream C, West Antarctica / S.F. Price, R.A. Bindschadler, C.L. Hulbe, I.R. Joughin. |
| Author(s): | Price, S. F. Bindschadler, R. A. Hulbe, C. L. Joughin, I. R. |
| Date: | 2001. |
| In: | Journal of Glaciology. (2001.), Vol. 47(157) (2001) |
| Abstract: | Presents two sets of observations and analysis; one from the region upstream of stagnant trunk of Ice Stream C and one concerning the interaction between Ice Streams C and B. Re- examines 'water piracy' hypothesis used to explain stagnation of Ice Stream C some 150 years ago. Examines how kinematic waves in upstream regions of Ice Stream C propagate ice thickening associated with stagnation. Contends that present day topography is the result, rather than cause of, stagnation, and that water piracy did not cause stagnation. Discusses flow features visible in SAR and visible imagery. Concludes that if upper regions of Ice Stream C continue to thicken and Ice Stream B continues to thin, then more ice will be diverted from the former to the latter. |
| Notes: | Journal of Glaciology. Vol. 47(157) :283-294 (2001). |
| Keywords: | 551.32 -- Glaciology. 551.324.29 -- Land ice, miscellaneous forms. 551.324.5 -- Land ice, flow. 621.396.96 -- Radar. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. (*767.3) -- Gould Coast. (*767.5) -- Siple Coast. |
| SPRI record no.: | 164646 |
LDR 01791naa#a2200000#a#4500 001 SPRI-164646 005 20240416182158.0 007 ta 008 240416s2001####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-164646 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aPost-stagnation behavior in the upstream regions of Ice Stream C, West Antarctica /‡cS.F. Price, R.A. Bindschadler, C.L. Hulbe, I.R. Joughin. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2001. 300 ## ‡ap. 283-294 :‡bill., diags. 500 ## ‡aJournal of Glaciology. Vol. 47(157) :283-294 (2001). 520 3# ‡aPresents two sets of observations and analysis; one from the region upstream of stagnant trunk of Ice Stream C and one concerning the interaction between Ice Streams C and B. Re- examines 'water piracy' hypothesis used to explain stagnation of Ice Stream C some 150 years ago. Examines how kinematic waves in upstream regions of Ice Stream C propagate ice thickening associated with stagnation. Contends that present day topography is the result, rather than cause of, stagnation, and that water piracy did not cause stagnation. Discusses flow features visible in SAR and visible imagery. Concludes that if upper regions of Ice Stream C continue to thicken and Ice Stream B continues to thin, then more ice will be diverted from the former to the latter. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324.29 -- Land ice, miscellaneous forms.‡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(*767.3) -- Gould Coast.‡2udc 651 #7 ‡a(*767.5) -- Siple Coast.‡2udc 700 1# ‡aPrice, S. F. 700 1# ‡aBindschadler, R. A. 700 1# ‡aHulbe, C. L. 700 1# ‡aJoughin, I. R. 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 47(157) (2001) ‡wSPRI-20534 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240416