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Record #104391:
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MARC recordA simple energy-balance model to calculate ice ablation at the margin of the Greenland ice sheet / Roger J. Braithwaite, Ole Oleson.
| Title: | A simple energy-balance model to calculate ice ablation at the margin of the Greenland ice sheet / Roger J. Braithwaite, Ole Oleson. |
| Author(s): | Braithwaite, Roger J. Oleson, Ole. |
| Date: | 1990. |
| In: | Journal of Glaciology. (1990.), Vol. 36(123) (1990) |
| Abstract: | Data for daily ice ablation on Nordbogletscher (1979-83) and Qamanârssûp sermia (1980-86) are used to test model which calculates ablation from climatic data. Mean errors are small: larger for Qamanârssûp sermia, which may be due to variations in ice albedo,, but model also underestimates ablation during Föhn events. Model suggests radiation accounts for 2/3 mean ablation for June-August at both sites, while turbulent fluxes account for 1/3. Average ablation rate is higher at Qamanârssûp sermia than at Nordbogletscher because both sensible-heat flux and short-wave radiation are higher. |
| Notes: | Journal of Glaciology. Vol. 36(123) :222-228 (1990). |
| Keywords: | 551.324.4 -- Land ice, mass and energy balance. 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.24 -- Ice sheets and caps. 551.324.43 -- Land ice, regime and mass balance. 551.324.433 -- Land ice, ablation and calving. 519.673 -- Modelling. E5 -- Glaciology: land ice. (*38) -- Greenland. (*324) -- Spitsbergen. |
| SPRI record no.: | 104391 |
LDR 01706naa#a2200000#a#4500 001 SPRI-104391 005 20231208195438.0 007 ta 008 231208s1990####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-104391 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aBraithwaite, Roger J. 245 12 ‡aA simple energy-balance model to calculate ice ablation at the margin of the Greenland ice sheet /‡cRoger J. Braithwaite, Ole Oleson. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 222-228 :‡bdiags., tables, map. 500 ## ‡aJournal of Glaciology. Vol. 36(123) :222-228 (1990). 520 3# ‡aData for daily ice ablation on Nordbogletscher (1979-83) and Qamanârssûp sermia (1980-86) are used to test model which calculates ablation from climatic data. Mean errors are small: larger for Qamanârssûp sermia, which may be due to variations in ice albedo,, but model also underestimates ablation during Föhn events. Model suggests radiation accounts for 2/3 mean ablation for June-August at both sites, while turbulent fluxes account for 1/3. Average ablation rate is higher at Qamanârssûp sermia than at Nordbogletscher because both sensible-heat flux and short-wave radiation are higher. 650 07 ‡a551.324.4 -- Land ice, mass and energy balance.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc 650 07 ‡a551.324.43 -- Land ice, regime and mass balance.‡2udc 650 07 ‡a551.324.433 -- Land ice, ablation and calving.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*38) -- Greenland.‡2udc 651 #7 ‡a(*324) -- Spitsbergen.‡2udc 700 1# ‡aOleson, Ole. 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 36(123) (1990) ‡wSPRI-20534 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231208