Sedimentological characteristics of the 2015 Tropical Cyclone Pam overwash sediments from Vanuatu, South Pacific

At Manuro (a mixed-carbonate embayment), the maximum flow height was 5.29 m mean sea level (MSL), with an inland extent of 106 m. The TC Pam sediments transition from a coarse to medium grained (mean: 1.07 Φ) carbonate sand (≤ 10 cm thick) to pumice (≤ 18 cm thick) that extends 400 m inland into Lake Otas. The TC Pam overwash sediments are characterized by a coarsening upward sequence (1.45 to 0.23 Φ) followed by a finer grained eolian cap. At Port Resolution Bay (a volcaniclastic beach, PRB), the maximum flow height was 3.30 m MSL (1.51 m flow depth), with an inland extent of 117 m. The TC Pam overwash sediments transition from a medium grained (mean: 1.76 Φ) volcanic sand (≤ 44 cm thick) to pumice (≤ 5 cm thick) that extends 320 m from the shoreline. A subtle fining upward sequence was present in trench PRB2, whereas PRB1, PRB3, and PRB4 contained TC Pam sediments that were laminated and showed little to no vertical gradation in grain size. At PRB, we applied an inverse sediment transport model to reconstruct maximum flow depths using laboratory derived settling velocities and the distance from the berm. The reconstructed flow depths at PRB2 (1.43 m), PRB3 (1.36 m), and PRB4 (1.34 m) compare favorably with the observed estimate (1.51 m), illustrating the applicability of the inverse sediment transport model to reconstruct flow depths of prehistoric landfalling TC's.