The advantage of our non-hydrostatic model over widely used non-dispersive shallow water models is that it can be used to capture wave dispersion

by including multiple vertical layers (Oishi et al., 2013, e.g.), Sotrastaurin mw but can also approximate the shallow water approach using a single layer to model the propagation of non-dispersive waves (Mitchell et al., 2010, e.g.). As the slide-tsunami scenarios we investigate here generate non-dispersive or very weakly dispersive waves our simulations generally use only a single layer. While this results in a (modest) computational overhead compared to alternative formulations, the benefit is that the results presented here can be directly compared with future

studies, using the same model, that examine highly dispersive waves generated by, for example, smaller slides Talazoparib in vivo (Glimsdal et al., 2013, e.g.). Mitchell et al. (2010) used the same model to study ancient tsunamis in the Jurassic Tethys sea, which shows the flexibility of the model in representing arbitrary coastlines. Here we describe how Fluidity has been modified to simulate slide-tsunami generation using prescribed rigid-block slide motion. This allows two of the four phases of slide-generated tsunami waves to be studied (Harbitz et al., 2006): the generation and propagation of the wave. The simulation of slide dynamics and tsunami wave inundation are not considered in this work. Previous studies of the Storegga slide tsunami did not directly include the effects of relative sea-level changes on bathymetry (Harbitz, 1992 and Bondevik et al., 2005). Isostatic adjustments from ice-sheet loading and unloading produce complex changes in relative sea-level across the region. Recent studies have simulated this process to produce 1000-year time slices of such changes since the Last Glacial Maximum (Bradley et al., 2011). Relative sea-level changes of up to 50 m have occurred since the Storegga slide, Mirabegron which caused substantial changes in

coastlines. For example, 8000 years ago a region in the southern North Sea was an island—Doggerland (Fitch et al., 2005)—and the coastlines around Norfolk, UK, and the northern coast of mainland Europe (Fig. 1) were dramatically different. Human artefacts (flints and spearheads) and mammal remains (mammoth and rhinoceros teeth) have been dredged from the Dogger Bank (Flemming, 2002). There has been speculation that the Storegga tsunami was the cause of the abandonment of the island by Mesolithic tribes (Weninger et al., 2008). In this paper, we first briefly describe the Fluidity model and the newly-implemented rigid-block slide model used to initiate the tsunami. We verify the implementation of this model by comparing our results to previous numerical results for test problems in both 2- and 3-dimensions.