Tsunami inundation and sediment transport in a sediment-limited embayment on American Samoa

Abstract Field observations and numerical simulations are used to explore tsunami inundation and sediment transport in an embayment (Fagafue Bay) on the north side of Tutuila, American Samoa during the 29 September 2009 South Pacific tsunami. Field observations of the nearshore bathymetry and topography, tsunami flow depth and sediment deposition, and extent of movable sandy sediment remaining on the beach were collected during two field surveys approximately two and five weeks after the tsunami. Onshore measurements of flow depth at forty-eight locations indicate the wave inundated almost 250 m onshore with a depth exceeding 7 m locally. The tsunami deposited patchy areas of sediment up to 0.2 m thick interspersed with a thin dusting (

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