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A numerical modeling approach for better differentiation of boulders transported by a tsunami, storm, and storm-induced energetic infragravity waves

A numerical modeling approach for better differentiation of boulders transported by a tsunami, storm, and storm-induced energetic infragravity waves
A numerical modeling approach for better differentiation of boulders transported by a tsunami, storm, and storm-induced energetic infragravity waves

Coastal boulders are often indicators of past extreme wave events. In fact, the coastal boulder distribution induced by infragravity-dominated storm waves (energetic IG waves) may be similar to that induced by tsunamis; however, this assumption is yet to be investigated. We show that the factors responsible for generating energetic IG waves under storm scenarios are not identical to those affecting the boulders' transport distances. Our results indicate that the storm waves typically only transport boulders over short distances as compared to boulders deposited by tsunamis, even when energetic IG waves are being generated. When the dimensionless transport distance of a boulder (=transport distance of a boulder/offshore wave height) is less than 4.0 × 10 over planar topography and 3.0 × 10 over reef topography, both waves can potentially be responsible for the transport distance. In this case, whether a reasonably-sized storm or tsunami can explain a boulder location in a study area should be investigated through detailed numerical modeling. We found a clear relationship between the dimensionless transport distance of tsunami boulders and the Iribarren number, and it is plausible to directly estimate offshore wave height or wavelength from the tsunami boulder distribution and beach slope without numerical simulation.

coastal boulder, identification, infragravity wave, numerical simulation, storm wave, tsunami
2169-9003
Watanabe, Masashi
880b3e5b-42a4-49a2-b196-0d06e54e45db
Goto, Kazuhisa
83ebddaf-a094-4138-b5d0-47d561e975e3
Roeber, Volker
919cc675-eb72-4f7a-b944-42f36a1c0499
Kan, Hironobu
a07a7c3a-2c22-4869-b9bc-48603f82bc03
Imamura, Fumihiko
13656bc7-ebb6-42c7-a49e-689e2a837a8f
Watanabe, Masashi
880b3e5b-42a4-49a2-b196-0d06e54e45db
Goto, Kazuhisa
83ebddaf-a094-4138-b5d0-47d561e975e3
Roeber, Volker
919cc675-eb72-4f7a-b944-42f36a1c0499
Kan, Hironobu
a07a7c3a-2c22-4869-b9bc-48603f82bc03
Imamura, Fumihiko
13656bc7-ebb6-42c7-a49e-689e2a837a8f

Watanabe, Masashi, Goto, Kazuhisa, Roeber, Volker, Kan, Hironobu and Imamura, Fumihiko (2023) A numerical modeling approach for better differentiation of boulders transported by a tsunami, storm, and storm-induced energetic infragravity waves. Journal of Geophysical Research: Earth Surface, 128 (9), [e2023JF007083]. (doi:10.1029/2023JF007083).

Record type: Article

Abstract

Coastal boulders are often indicators of past extreme wave events. In fact, the coastal boulder distribution induced by infragravity-dominated storm waves (energetic IG waves) may be similar to that induced by tsunamis; however, this assumption is yet to be investigated. We show that the factors responsible for generating energetic IG waves under storm scenarios are not identical to those affecting the boulders' transport distances. Our results indicate that the storm waves typically only transport boulders over short distances as compared to boulders deposited by tsunamis, even when energetic IG waves are being generated. When the dimensionless transport distance of a boulder (=transport distance of a boulder/offshore wave height) is less than 4.0 × 10 over planar topography and 3.0 × 10 over reef topography, both waves can potentially be responsible for the transport distance. In this case, whether a reasonably-sized storm or tsunami can explain a boulder location in a study area should be investigated through detailed numerical modeling. We found a clear relationship between the dimensionless transport distance of tsunami boulders and the Iribarren number, and it is plausible to directly estimate offshore wave height or wavelength from the tsunami boulder distribution and beach slope without numerical simulation.

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More information

Accepted/In Press date: 20 August 2023
e-pub ahead of print date: 28 August 2023
Published date: 1 September 2023
Additional Information: Publisher Copyright: © 2023. American Geophysical Union. All Rights Reserved.
Keywords: coastal boulder, identification, infragravity wave, numerical simulation, storm wave, tsunami

Identifiers

Local EPrints ID: 493922
URI: http://eprints.soton.ac.uk/id/eprint/493922
ISSN: 2169-9003
PURE UUID: 788d2800-baad-4be2-adc3-52444af9fe8f
ORCID for Masashi Watanabe: ORCID iD orcid.org/0000-0003-3670-7385

Catalogue record

Date deposited: 17 Sep 2024 16:58
Last modified: 19 Sep 2024 02:09

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Contributors

Author: Masashi Watanabe ORCID iD
Author: Kazuhisa Goto
Author: Volker Roeber
Author: Hironobu Kan
Author: Fumihiko Imamura

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