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Record #123615:
- #123615
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MARC recordPhotogrammetric analysis of 1984-89 surface altitude change of the partially debris-covered Eliot Glacier, Mount Hood, Oregon, U.S.A. / S.C. Lundstrom, A.E. McCafferty, J.A. Coe.
| Title: | Photogrammetric analysis of 1984-89 surface altitude change of the partially debris-covered Eliot Glacier, Mount Hood, Oregon, U.S.A. / S.C. Lundstrom, A.E. McCafferty, J.A. Coe. |
| Author(s): | Lundstrom, S. C. McCafferty, A. E. Coe, J. A. |
| Date: | 1993. |
| In: | Annals of Glaciology. (1993.), Vol. 17 (1993) |
| Abstract: | Analysis indicates average thinning of ablation area of 4.2 m during 1984-89. Thinning is generally more marked near equilibrium line, where debris cover is absent, than on lower part of glacier, where supraglacial debris is thicker than 1 m. Pattern of change is partly related to reduction of ablation with increasing debris thickness, but flow kinematics are also important when considering changes in ice thickness. |
| Notes: | Annals of Glaciology. Vol. 17 :167-170 (1993). |
| Keywords: | 551.32 -- Glaciology. 53.087.23 -- Remote sensing. 528.715 -- Aerial surveys. 551.324 -- Land ice. 551.324.22 -- Glaciers. 551.324.83 -- Land ice, load. E5 -- Glaciology: land ice. (73) -- United States. (79) -- Pacific states. |
| SPRI record no.: | 123615 |
LDR 01484naa#a2200000#a#4500 001 SPRI-123615 005 20240418143450.0 007 ta 008 240418s1993####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-123615 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aLundstrom, S. C. 245 10 ‡aPhotogrammetric analysis of 1984-89 surface altitude change of the partially debris-covered Eliot Glacier, Mount Hood, Oregon, U.S.A. /‡cS.C. Lundstrom, A.E. McCafferty, J.A. Coe. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 167-170 :‡bill., diag., maps. 500 ## ‡aAnnals of Glaciology. Vol. 17 :167-170 (1993). 520 3# ‡aAnalysis indicates average thinning of ablation area of 4.2 m during 1984-89. Thinning is generally more marked near equilibrium line, where debris cover is absent, than on lower part of glacier, where supraglacial debris is thicker than 1 m. Pattern of change is partly related to reduction of ablation with increasing debris thickness, but flow kinematics are also important when considering changes in ice thickness. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a53.087.23 -- Remote sensing.‡2udc 650 07 ‡a528.715 -- Aerial surveys.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.22 -- Glaciers.‡2udc 650 07 ‡a551.324.83 -- Land ice, load.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(73) -- United States.‡2udc 651 #7 ‡a(79) -- Pacific states.‡2udc 700 1# ‡aMcCafferty, A. E. 700 1# ‡aCoe, J. A. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 17 (1993) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418