Tsunami shoaling and run-up in the Large Wave Flume of ... - FZK
Tsunami shoaling and run-up in the Large Wave Flume of ... - FZK
Tsunami shoaling and run-up in the Large Wave Flume of ... - FZK
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DFG – Roundtable <strong>Tsunami</strong> April 23-24, 2007, Hannover<br />
Source Area<br />
C<br />
Offshore Offshore<br />
Scheme <strong>of</strong> <strong>Tsunami</strong> <strong>Wave</strong> Propagation<br />
Propagation towards Shorel<strong>in</strong>e<br />
C<br />
C<br />
Shelf<br />
Most important <strong>Tsunami</strong> effects occur at near- & onshore areas<br />
due to hydraulic performance <strong>of</strong> <strong>Tsunami</strong> waves:<br />
Near- & Onshore<br />
- Shoal<strong>in</strong>g, - reflection, - transmission, - break<strong>in</strong>g, - <strong>run</strong>-<strong>up</strong> & overtopp<strong>in</strong>g, - backwash,<br />
penetration <strong>and</strong> <strong>in</strong>undation <strong>in</strong>to settlements
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