Fig. 2: Simulated tsunami surface elevation (blue line) and flow velocity down to about 1–10 m above the sea floor (dotted) during the Storegga tsunami at the location of marine sediment cores with an 8.2 ka layer. | Nature Communications

Fig. 2: Simulated tsunami surface elevation (blue line) and flow velocity down to about 1–10 m above the sea floor (dotted) during the Storegga tsunami at the location of marine sediment cores with an 8.2 ka layer.

From: Contamination of 8.2 ka cold climate records by the Storegga tsunami in the Nordic Seas

Fig. 2

Paleo-water depths in brackets. For core locations, see Fig. 1. a Core site MD95-2011 at the Vøring plateau in the Norwegian Sea. b Core site LINK14 east of the Faroe Island and c Core site Troll, 28-03 in the Norwegian channel. Source data are available at https://doi.org/10.18710/6KDQ7I.

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