Jökull


Jökull - 01.10.1998, Page 40

Jökull - 01.10.1998, Page 40
Vatnajökull which flows from an elevation of 1990 m of Bárðarbunga to 730 m; an outlet with an exception- al area distribution as 410 km2 or 40% of the total area is located between 1500 m and 1700 m elevation. Second, Brúarjökull, the largest of the northern out- lets of Vatnajökull flowing with a low slope from an elevation of 1930 m to 580 m over a distance of 55 km. The Grímsvötn drainage basin is located in the central area of the ice cap where ice drains into a de- pression created by a subglacial geothermal area con- tinuously melting ice (Björnsson, 1988). All the drainage basins except Brúarjökull are located within the active volcanic zone and abundant ash cover en- hances melting in the ablation areas. Point measurements were done on Örœfajökull at an elevation of 1800 m a. s. 1. in last the two last years considered in this report. Meltwater from these glaciers drains to some of the main river systems of Iceland (Fig. 1, Table 2). Hveifis- fljót drains Síðujökull, Tungnaá Tungnaárjökull, Kaldakvísl Köldukvíslarjökull, and Jökulsá á Fjöllum drains Dyngjujökull. Two major river systems: Kreppal Kverká and Jökulsá á Brú drain Brúarjökull. The dis- charge of the glacial rivers is monitored by the Nation- al Energy Authority at streamflow gauges some dis- tance from the glacier (Fig. 1). The location of the sta- tions and the total area of the river basins, including the glaciers, is given in Table 1. At the discharge gauges the percentage of the drainage basins covered by glaciers is 12 for Tungnaá, 43 for Kaldakvísl, 57 for Jökulsá á Fjöllum and 67 for Jökulsá á Brú. The rivers Tungnaá, Kaldakvísl and Jökulsá á area (km ) 20 40 area (km ) 20 40 area (km ) 20 40 area (km ) 20 40 2000 1600 0 200 400 cumulative area (km2) 0 200 400 cumulative area (km2) area (km2) 0 200 400 cumulative area (km2) 0 200 400 cumulative area (km2) area (km2) Fig. 3. Area distribution with elevation of several glacier drainage basins of Vatna- jökull. - Flatarmálsdreifing nokkurra skriðjökla með hœð. 0 40 80 120 0 40 80 120 160 cumulative area (km2) cumulative area (km2) 38 JOKULL, No. 45, 1998
Page 1
Page 2
Page 3
Page 4
Page 5
Page 6
Page 7
Page 8
Page 9
Page 10
Page 11
Page 12
Page 13
Page 14
Page 15
Page 16
Page 17
Page 18
Page 19
Page 20
Page 21
Page 22
Page 23
Page 24
Page 25
Page 26
Page 27
Page 28
Page 29
Page 30
Page 31
Page 32
Page 33
Page 34
Page 35
Page 36
Page 37
Page 38
Page 39
Page 40
Page 41
Page 42
Page 43
Page 44
Page 45
Page 46
Page 47
Page 48
Page 49
Page 50
Page 51
Page 52
Page 53
Page 54
Page 55
Page 56
Page 57
Page 58
Page 59
Page 60
Page 61
Page 62
Page 63
Page 64
Page 65
Page 66
Page 67
Page 68
Page 69
Page 70
Page 71
Page 72
Page 73
Page 74
Page 75
Page 76
Page 77
Page 78
Page 79
Page 80
Page 81
Page 82
Page 83
Page 84
Page 85
Page 86
Page 87
Page 88
Page 89
Page 90
Page 91
Page 92
Page 93
Page 94
Page 95
Page 96
Page 97
Page 98
Page 99
Page 100
Page 101
Page 102
Page 103
Page 104
Page 105
Page 106
Page 107
Page 108
Page 109
Page 110
Page 111
Page 112

x

Jökull

Direct Links

If you want to link to this newspaper/magazine, please use these links:

Link to this newspaper/magazine: Jökull
https://timarit.is/publication/1155

Link to this issue:

Link to this page:

Link to this article:

Please do not link directly to images or PDFs on Timarit.is as such URLs may change without warning. Please use the URLs provided above for linking to the website.