accumulation during winter, and thus
more wintertime runoff and smaller spring floods.
Model calculations indicate
that further changes in the seasonal cycle of runoff may be expected.Mass loss of the glaciers has
led to crustal
uplift in much of the interior of Iceland and near the south-east and southern
coast. South of the Vatnajökull ice cap, the measured uplift exceeds 20 mm/year
/climatology/iceland/climate-report