Jökull


Jökull - 01.10.1998, Page 48

Jökull - 01.10.1998, Page 48
Table 6. Mass balance of drainage basins in Vatnajökull, 1993-1994. Bw and bw = winter balance, Bs and bs = summer balance, Bn and bn = net balance, ELA = the equilibrium line altitude, AAR = accumulation area ratio. Accuracy 15%. -Afkoma skriðjökla Vatnajökuls, 1993-1994. Bw og bw er vetrarafkoma, Bs and bs er sumarafkoma, Bn og bn ársafkoma, ELA er hœð jafnvœgislínu, AAR er hlutfall ákomusvœðis af heildarflatarmáli jökuls. Nákvœmni 15%. Area Bw Bs B„ bw bs b„ ELA AAR kmJ 106m3 10‘m3 106m3 m a'1 m a'1 ma'1 m Tungnaárjökull 308 525 -565 -40 1.70 -1.84 -0.14 1160 0.60 Köldukvíslarjökull 313 c. 450 c. -460 c. -10 c. 1.43 c. -1.47 c. -0.03 1300 0.55 Dyngjujökull 1040 1495 -1305 190 1.44 -1.25 0.19 1250 0.71 Brúarjökull 1695 2965 -2490 475 1.75 -1.47 0.28 1140 0.67 Grímsvötn 160 350 -85 265 2.19 -0.59 1.60 1.0 Fig. 9. Mass balance measurements, 1993-1994; Specific mass balance in m water equivalent, bw: winter balance, bs: summer balance, bn: annual net balance. -Afkoma 1993-1994 sem metrar vatns. bw: vetrarafkoma, bs: sumarafkoma, b„: ársafkoma. Mœlistaðir eru merktir með krossi. northem than the westem outlets and, for the glacier outlets as a whole, the summer balance was more negative on the westem than on the northem outlets. The snowfall increased the albedo and caused an ex- ceptionally sharp difference in the summer balance gradient between the accumulation areas and abla- tion areas similar to the summer of 1992. Moreover, the ice surface emerged earlier in the summer in the western part of the ablation area of Brúarjökull than in the eastern part. The maximum values of the sum- mer balance were estimated -5600 mm at 700 m on Tungnaárjökull, -5300 mm at 600 m on Brúarjökull and -4500 mm at 750 m on Dyngjujökull. The specific net balance in the central area of the ice cap was about 3000 mm. Integrated over the area of the glaciers, the net balance of all the glaciers was positive (Figs. 6 and 7), especially on the northern outlets where the specific mass balance was more 46 JÖKULL, No. 45, 1998
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