The discharge was measured twice: The flood that began at Gígjökull at around 11:30, reached a peak discharge of 250 m3/s two hours later at the old bridge. Both 28 and
29 April, mean discharge from Gígjökull was 130-150 m3/s, which was higher than the days before.
Additionally, the electrical conductivity of Krossá and Steinholtsá rivers remained high.
For more photos of the hydrological
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