lllwtmte the fiercrd
sfirulation results in muhiple wuys. The simple
graph format (Fig. 8) is complimentary to the 3D visualisations,
and shovs sensitivity of the predicted inundation, to the pre-
scribed sea Ievel inputs. This affords a more pragmatic view of
extreme events and scenarios, which informed stakeholders can
use to discuss adaptation. This was especially imporant when
previous assumptions are challenged by new obsenations (e.g.
in Yarmouttr, nanr surge maxima following the 2013/14 storms).