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Request for Proposals – North Atlantic Tsunamis<br />

North Atlantic tsunamis have exhibited a low frequency; however, tsunamis have been documented to<br />

occur, which could generate catastrophic losses along Atlantic coastlines today (Baptista et al, 2011).<br />

Tsunami Hazard assessments for various regions have been made based on historical data, with a view<br />

to protecting life, and estimating economic damage to property and infrastructure (Dunbar and Weaver,<br />

2008; Leonard et al, 2012). However, the complexities <strong>of</strong> tsunami inundation dictate that multiple scales<br />

be examined via numerical simulation when trying to assess the potential damage footprint (Lynnett<br />

and Liu, 2011) for catastrophe risk modeling purposes.<br />

Adding to the complexity <strong>of</strong> tsunami risk is the potential for submarine landslide events to trigger<br />

tsunami inundation (ten Brink et al, 2007) without an accompanying earthquake (the peril with which<br />

tsunamis are <strong>of</strong>ten paired in catastrophe models). Referring to catastrophe risk modeling, Lotz and<br />

Schmiesing (2012) state that “no vendor model currently exists for quantifying tsunami risk.”<br />

Excerpt: ten Brink, 2009: Fig. 1.<br />

Shaded relief map <strong>of</strong> the East<br />

Coast <strong>of</strong> the United States with<br />

interpretation. NC — Norfolk<br />

Canyon, WC — Wilmington<br />

Canyon, HC — Hudson Canyon, VC<br />

— Veatch Canyon. Inset —<br />

Location map. NES — New<br />

England Seamounts. BS — Blake<br />

Spur, BE — Blake Escarpment.<br />

Seafloor data on the continental<br />

slope and rise is almost entirely<br />

based on multibeam bathymetry,<br />

w<strong>here</strong>as the majority <strong>of</strong> seafloor<br />

data on the shelf is based on<br />

single-beam bathymetry. Figure<br />

courtesy <strong>of</strong> David Twichell (USGS).<br />

Excerpt: ten Brink, 2009: Assessment <strong>of</strong> tsunami hazard to the Atlantic coast <strong>of</strong> the Unites States poses a scientific<br />

challenge because <strong>of</strong> the paucity <strong>of</strong> both historical events and prehistoric tsunami evidence. The Atlantic coast <strong>of</strong><br />

the U.S., also known as the U.S. East Coast, is highly vulnerable to tsunami damage because major population<br />

centers and industrial facilities are located near the shoreline at low-lying elevations.<br />

RPI is interested in generating a set <strong>of</strong> damage or vulnerability functions from modeled Atlantic tsunami<br />

inundations impacting Atlantic coastlines with large potential for catastrophic losses. In addition, we are<br />

keen to develop an event set <strong>of</strong> damage scenarios from existing high quality research with a view to<br />

quantifying loss probabilistically.<br />

The <strong>Risk</strong> <strong>Prediction</strong> <strong>Initiative</strong> (RPI2.0), part <strong>of</strong> the <strong>Bermuda</strong> <strong>Institute</strong> <strong>of</strong> <strong>Ocean</strong> <strong>Sciences</strong>, promotes productive dialogue between<br />

scientists and (re)insurers involved in catastrophe risk by refocusing scientific research towards answering the industry’s questions.<br />

BIOS is an independent U.S. non-pr<strong>of</strong>it marine research and educational institute and <strong>Bermuda</strong> registered charity founded in 1903.


Questions, objectives and scope <strong>of</strong> work<br />

Develop a set <strong>of</strong> realistic tsunami inundation scenarios, to a high resolution, for high exposure regions<br />

along Atlantic coastlines.<br />

Develop and provide a probabilistic mechanism for determining the proportion <strong>of</strong> earthquake-induced<br />

tsunamis and tele-tsunamis, vs. non-earthquake tsunami genesis (e.g. from local submarine landslides).<br />

Key components <strong>of</strong> this work will be:<br />

- A final report that details the results <strong>of</strong> the analysis. The final report should stress the thinking<br />

and rationale supporting the techniques that were used to analyze and clean the primary data<br />

as well as the final analysis <strong>of</strong> the finalized data set.<br />

- A dataset derived from the study which underpins any subsequent publications and/or code<br />

which may be used directly by RPI members prior to any resulting publication.<br />

This work should be completed by June 2014. The successful scientist(s) should plan to attend an RPI<br />

Research Update Workshop in <strong>Bermuda</strong> in 2014, with a view to a presentation <strong>of</strong> the results. The<br />

successful scientist(s) may also be requested to attend other RPI Members functions.<br />

Interested parties should submit a research proposal <strong>of</strong> no more than 5 pages that includes a budget.<br />

Proposals should be uploaded electronically via the following website:<br />

http://rpi.bios.edu/proposal_upload/upload.<br />

Previous RPI grant awards have generally been on the order <strong>of</strong> $50K/year. Award decisions are based on<br />

the scientific merit <strong>of</strong> the proposed research, the relevance <strong>of</strong> the research to the stated goals,<br />

development and availability <strong>of</strong> appropriate follow-on applications for our Members, and the dollar<br />

amount requested.<br />

Further information on the RPI is available at http://rpi.bios.edu/.<br />

Submissions deadline is May 15, 2013.


References<br />

Baptista, M. A., J. M. Miranda, R. Omira, and C. Antunes Potential inundation <strong>of</strong> Lisbon downtown by a<br />

1755-like tsunami, Nat. Hazards Earth Syst. Sci., 11, 3319–3326, 2011<br />

www.nat-hazards-earth-syst-sci.net/11/3319/2011/ doi:10.5194/nhess-11-3319-2011<br />

Dunbar, Paula K. and Craig S. Weaver, U.S. States and Territories National Tsunami Hazard Assessment:<br />

Historical Record and Sources for Waves, Prepared for the, National Tsunami Hazard Mitigation<br />

Program, August 2008 U.S. DEPARTMENT OF COMMERCE, National <strong>Ocean</strong>ic and Atmospheric<br />

Administration, U.S. DEPARTMENT OF INTERIOR, U.S. Geological Survey<br />

Leonard, L.J., G.C. Rogers, and S. Mazzotti, A Preliminary Tsunami Hazard Assessment <strong>of</strong> the Canadian<br />

Coastline, OPEN FILE 7201, GEOLOGICAL SURVEY OF CANADA, 2012, Natural Resources Canada.<br />

Lotz, L., and Schmiesing, Z., Frequent Changes to Catastrophe Models: The Far-Reaching Impact ,<br />

Emphasis 2012 - Issue 1, March 2012, Towers Watson,<br />

http://www.towerswatson.com/en/Insights/Newsletters/Global/emphasis<br />

Lynett, P., and Liu, P. L.-F. (2011) "Simulation <strong>of</strong> Complex Tsunami Behavior." Computing in Science and<br />

Engineering Magazine, July/August 2011, v. 13(4), pp. 50-57, doi: 10.1109/ MCSE.2011.22.<br />

ten Brink, Uri, Preface - Tsunami hazard along the U.S. Atlantic coast, Marine Geology 264 (2009) 1–3<br />

_____, David Twichell, Eric Geist, Jason Chaytor, Jacques Locat, Homa Lee, Brian Buczkowski, and<br />

Mylène Sansoucy (Atlantic and Gulf <strong>of</strong> Mexico Tsunami Hazard Assessment Group), The Current State <strong>of</strong><br />

Knowledge Regarding Potential Tsunami Sources Affecting U.S. Atlantic and Gulf Coasts - A Report to the<br />

Nuclear Regulatory Commission, USGS, 2007

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