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Record #112071:
- #112071
Main publication details
MARC recordModelling englacial temperatures for Jakobshavns Isbrae / Martin Funk, Almut Iken, Keith Echelmeyer, William D. Harrison.
| Title: | Modelling englacial temperatures for Jakobshavns Isbrae / Martin Funk, Almut Iken, Keith Echelmeyer, William D. Harrison. |
| Author(s): | Funk, Martin. Iken, Almut. Echelmeyer, Keith. Harrison, William D. |
| 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. Complex temperature regime caused by rapid flow of ice stream. Temperature model solves two-dimensional steady-state temperature field for prescribed surface and bed topography. Model is applied to flow along centre line in ice stream as well as to flow in ice sheet, well outside stream. Main difference is appearance of more pronounced temperate layer in stream than in sheet. |
| Notes: | Eos : transactions, American Geophysical Union. Vol. 72(44, supplement) :150 (1991). |
| Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.22 -- Glaciers. 551.324.412 -- Land ice, temperature: Jakobshavn Isbrae. E5 -- Glaciology: land ice. (*38) -- Greenland. (*384) -- West Greenland. (*384.42) -- Ilulissat/Jakobshavn. |
| SPRI record no.: | 112071 |
LDR 01522naa#a2200000#a#4500 001 SPRI-112071 005 20230329201811.0 007 ta 008 230329s1991####xx####|##|###|0||#0|eng#d 035 ## ‡aSPRI-112071 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aModelling englacial temperatures for Jakobshavns Isbrae /‡cMartin Funk, Almut Iken, Keith Echelmeyer, William D. Harrison. 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. Complex temperature regime caused by rapid flow of ice stream. Temperature model solves two-dimensional steady-state temperature field for prescribed surface and bed topography. Model is applied to flow along centre line in ice stream as well as to flow in ice sheet, well outside stream. Main difference is appearance of more pronounced temperate layer in stream than in sheet. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.22 -- Glaciers.‡2udc 650 07 ‡a551.324.412 -- Land ice, temperature: Jakobshavn Isbrae.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*38) -- Greenland.‡2udc 651 #7 ‡a(*384) -- West Greenland.‡2udc 651 #7 ‡a(*384.42) -- Ilulissat/Jakobshavn.‡2udc 700 1# ‡aFunk, Martin. 700 1# ‡aIken, Almut. 700 1# ‡aEchelmeyer, Keith. 700 1# ‡aHarrison, William D. 773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 72(44, supplement) (1991) ‡wSPRI-1028 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230329