HARMONIE model terrain elevation.
Vatnajökull), as well as Hágöngulón and a group of lakes around Kvíslavatn in the Sprengisan-
dur region between Vatnajökull and Hofsjökull. Also missing in the model are some main water
courses (class 511;
789 km2, 0.8%), most notably the wide southern outflow from Vatnajökull.
The main problem with the model characterisation of surface type is the overestimation
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf