SPRI library catalogue
View a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #104087:
Potential for basal melting under the Summit coring site, central Greenland (abstract) / John Firestone, E.D. Waddington, J. Cunningham.
Title: | Potential for basal melting under the Summit coring site, central Greenland (abstract) / John Firestone, E.D. Waddington, J. Cunningham. |
Author(s): | Firestone, John. Waddington, E. D. Cunningham, J. |
Date: | 1990. |
In: | Annals of Glaciology. (1990.), Vol. 14 (1990) |
Abstract: | Climatic record from Greenland bore holes may extend beyond last interglacial only if basal ice near drilling site has never reached its pressure melting point (-2°C). Results of analysis of measurements from Summit site showed that basal ice does not melt if geothermal flux is <54 mW m⁻², using same mass balance and temperature histories as previous study at Crête where value of 48 mW m⁻² was estimated. |
Notes: | Annals of Glaciology. Vol. 14 :334 (1990). |
Keywords: | 551.324.433 -- Land ice, ablation and calving. 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.412 -- Land ice, temperature. E5 -- Glaciology: land ice. (*38) -- Greenland. |
SPRI record no.: | 104087 |
LDR 01311naa#a2200000#a#4500 001 SPRI-104087 005 20231207192051.0 007 ta 008 231207s1990####xx####|##|###|0||#0|eng#d 035 ## ‡aSPRI-104087 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aFirestone, John. 245 10 ‡aPotential for basal melting under the Summit coring site, central Greenland (abstract) /‡cJohn Firestone, E.D. Waddington, J. Cunningham. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 334. 500 ## ‡aAnnals of Glaciology. Vol. 14 :334 (1990). 520 3# ‡aClimatic record from Greenland bore holes may extend beyond last interglacial only if basal ice near drilling site has never reached its pressure melting point (-2°C). Results of analysis of measurements from Summit site showed that basal ice does not melt if geothermal flux is <54 mW m⁻², using same mass balance and temperature histories as previous study at Crête where value of 48 mW m⁻² was estimated. 650 07 ‡a551.324.433 -- Land ice, ablation and calving.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.412 -- Land ice, temperature.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*38) -- Greenland.‡2udc 700 1# ‡aWaddington, E. D. 700 1# ‡aCunningham, J. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 14 (1990) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231207