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Twin Tsunamis Triggered by the 12 January 2010 Haiti Earthquake

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TLDR
The International Tsunami Survey Team (ITST) was deployed within weeks of the Haiti earthquake and covered the greater Bay of Port-au-Prince and more than 100 km of Hispaniola's southern coastline as mentioned in this paper.
Abstract
On 12 January 2010, a magnitude M w 7.0 earthquake occurred 25 km west–southwest of Haiti’s capital Port-au-Prince causing an estimated 316,000 fatalities, thereby exceeding any previous loss of life from a similar size earthquake. In addition, tsunami waves triggered by the earthquake caused at least three fatalities at Petit Paradis due to a complete lack of tsunami awareness. The International Tsunami Survey Team (ITST) was deployed within weeks of the event and covered the greater Bay of Port-au-Prince and more than 100 km of Hispaniola’s southern coastline. The collected survey data include more than 21 tsunami heights along with observations of coastal land level change. Maximum tsunami heights of 3 m have been measured for two independently triggered tsunamis.

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Citations
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Physical modeling of tsunamis generated by three-dimensional deformable granular landslides

TL;DR: In this paper, a pneumatic landslide generator was used to generate a 3D tsunami wave based on the generalized Froude similarity, and the wave amplitudes, periods, and wavelengths were related to the landslide parameters at impact.
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A two-layer granular landslide model for tsunami wave generation: Theory and computation

TL;DR: In this paper, a two-layer model for granular landslide motion and tsunami wave generation is developed and tested using a depth-averaged coordinate system, taking into account the dynamic interaction between the lower-layer granular landslides and upper-layer water motion.
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A simplified 3-D Navier-Stokes numerical model for landslide-tsunami: Application to the Gulf of Mexico

TL;DR: In this article, a simplified 3D Navier-Stokes (3D NS) model for two fluids, water and landslide material (mudslide), is presented and validated with standard laboratory experiments.
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Physical modelling of tsunamis generated by three-dimensional deformable granular landslides on planar and conical island slopes

TL;DR: Predictive equations for the offshore propagating wave amplitudes, periods, celerities and lengths generated by landslides on planar and divergent convex conical hill slopes are derived, which allow an initial rapid tsunami hazard assessment.
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Tsunami deposits of the Caribbean – Towards an improved coastal hazard assessment

TL;DR: In this paper, the authors reviewed almost 60 sites for possible geological evidence of tsunamis in the Caribbean including fine-grained subsurface deposits and subaerial coarse clasts, and re-evaluated their implications for tsunami hazard assessment against state-of-the-art models of onshore sediment deposition by tsunami and extreme storms.
References
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Journal ArticleDOI

Numerical Modeling of Tidal Wave Runup

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Possible criteria for predicting earthquake locations and their application to major plate boundaries of the Pacific and the Caribbean

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The run-up of N-waves on sloping beaches

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