FN Archimer Export Format PT J TI Tsunamis caused by submarine slope failures along western Great Bahama Bank BT AF SCHNYDER, Jara S. D. EBERLI, Gregor P. KIRBY, James T. SHI, Fengyan TEHRANIRAD, Babak MULDER, Thierry DUCASSOU, Emmanuelle HEBBELN, Dierk WINTERSTELLER, Paul AS 1:1;2:1;3:2;4:2;5:2;6:3;7:3;8:4;9:4; FF 1:;2:;3:;4:;5:;6:;7:;8:;9:; C1 Univ Miami, CSL Ctr Carbonate Res, 4600 Rickenbacker Cswy, Miami, FL 33149 USA. Univ Delaware, Ctr Appl Coastal Res, Newark, DE 19716 USA. Univ Bordeaux, UMR EPOC 5805, F-33615 Pessac, France. Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany. C2 UNIV MIAMI, USA UNIV DELAWARE, USA UNIV BORDEAUX, FRANCE UNIV BREMEN MARUM, GERMANY IF 4.259 TC 29 UR https://archimer.ifremer.fr/doc/00506/61772/65754.pdf https://archimer.ifremer.fr/doc/00506/61772/65755.pdf https://archimer.ifremer.fr/doc/00506/61772/65756.mov https://archimer.ifremer.fr/doc/00506/61772/65757.mov https://archimer.ifremer.fr/doc/00506/61772/65758.mov LA English DT Article CR CARAMBAR BO Le SuroƮt AB Submarine slope failures are a likely cause for tsunami generation along the East Coast of the United States. Among potential source areas for such tsunamis are submarine landslides and margin collapses of Bahamian platforms. Numerical models of past events, which have been identified using high-resolution multibeam bathymetric data, reveal possible tsunami impact on Bimini, the Florida Keys, and northern Cuba. Tsunamis caused by slope failures with terminal landslide velocity of 20 ms(-1) will either dissipate while traveling through the Straits of Florida, or generate a maximum wave of 1.5 m at the Florida coast. Modeling a worst-case scenario with a calculated terminal landslide velocity generates a wave of 4.5 m height. The modeled margin collapse in southwestern Great Bahama Bank potentially has a high impact on northern Cuba, with wave heights between 3.3 to 9.5 m depending on the collapse velocity. The short distance and travel time from the source areas to densely populated coastal areas would make the Florida Keys and Miami vulnerable to such low-probability but high-impact events. PY 2016 PD NOV SO Scientific Reports SN 2045-2322 PU Nature Publishing Group VL 6 IS 35925 UT 000387011200001 DI 10.1038/srep35925 ID 61772 ER EF