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Modeling boulder transport by coastal waves on cliff topography: Case study at Hachijo Island, Japan

Modeling boulder transport by coastal waves on cliff topography: Case study at Hachijo Island, Japan
Modeling boulder transport by coastal waves on cliff topography: Case study at Hachijo Island, Japan

Clifftop coastal boulders transported by storm waves or tsunamis have been reported around the world. Although numerical calculation of boulder transport is a strong tool for the identification of tsunami or storm boulders, and for estimation of the wave size emplacing boulders, models which can reasonably solve boulder transport from below a cliff or from a cliff-edge onto a cliff-top do not yet exist. In this study, we developed a new numerical formulation for cliff-top deposition of boulders from the cliff edge or below the cliff, with validation from laboratory tests. We then applied the model using storm and tsunami wave forcing to simulate the observed boulder deposits at the northwest coast of Hachijo Island, Japan. Using the model, the actual distribution of boulders was explained well using a reasonable storm wave height without assumption of anomalously high-water level by storm surge. Results show that boulder transport from the cliff edge or under the cliff onto the cliff-top was possible from a tsunami with periods of 5~10 min or storm waves with no storm surge. However, the actual distribution of boulders on the cliff was explained only by storm waves, but not by tsunami. Therefore, the boulders distributed at this site are likely of storm wave origin. Our developed model for the boulder transport calculation can be useful for identifying a boulder's origin and can reasonably calculate cliff-top deposition of boulders by tsunami and storm waves.

boulder transport model, cliff-top deposition, identification of tsunami or storm boulder, numerical simulation, wave-tank experiment
0197-9337
2939-2956
Watanabe, Masashi
880b3e5b-42a4-49a2-b196-0d06e54e45db
Goto, Kazuhisa
83ebddaf-a094-4138-b5d0-47d561e975e3
Imamura, Fumihiko
13656bc7-ebb6-42c7-a49e-689e2a837a8f
Kennedy, Andrew
82f2948b-45ec-4177-aa7a-87d8cb1dfcdc
Sugawara, Daisuke
c1b6a01e-4597-4ced-9295-2687322d6e03
Nakamura, Norihiro
d51546a4-8866-4003-b416-aefb1c7edbe1
Tonosaki, Takayuki
3ac6d7b4-9219-41ed-9453-f5e70d4d5d7c
Watanabe, Masashi
880b3e5b-42a4-49a2-b196-0d06e54e45db
Goto, Kazuhisa
83ebddaf-a094-4138-b5d0-47d561e975e3
Imamura, Fumihiko
13656bc7-ebb6-42c7-a49e-689e2a837a8f
Kennedy, Andrew
82f2948b-45ec-4177-aa7a-87d8cb1dfcdc
Sugawara, Daisuke
c1b6a01e-4597-4ced-9295-2687322d6e03
Nakamura, Norihiro
d51546a4-8866-4003-b416-aefb1c7edbe1
Tonosaki, Takayuki
3ac6d7b4-9219-41ed-9453-f5e70d4d5d7c

Watanabe, Masashi, Goto, Kazuhisa, Imamura, Fumihiko, Kennedy, Andrew, Sugawara, Daisuke, Nakamura, Norihiro and Tonosaki, Takayuki (2019) Modeling boulder transport by coastal waves on cliff topography: Case study at Hachijo Island, Japan. Earth Surface Processes and Landforms, 44 (15), 2939-2956. (doi:10.1002/esp.4684).

Record type: Article

Abstract

Clifftop coastal boulders transported by storm waves or tsunamis have been reported around the world. Although numerical calculation of boulder transport is a strong tool for the identification of tsunami or storm boulders, and for estimation of the wave size emplacing boulders, models which can reasonably solve boulder transport from below a cliff or from a cliff-edge onto a cliff-top do not yet exist. In this study, we developed a new numerical formulation for cliff-top deposition of boulders from the cliff edge or below the cliff, with validation from laboratory tests. We then applied the model using storm and tsunami wave forcing to simulate the observed boulder deposits at the northwest coast of Hachijo Island, Japan. Using the model, the actual distribution of boulders was explained well using a reasonable storm wave height without assumption of anomalously high-water level by storm surge. Results show that boulder transport from the cliff edge or under the cliff onto the cliff-top was possible from a tsunami with periods of 5~10 min or storm waves with no storm surge. However, the actual distribution of boulders on the cliff was explained only by storm waves, but not by tsunami. Therefore, the boulders distributed at this site are likely of storm wave origin. Our developed model for the boulder transport calculation can be useful for identifying a boulder's origin and can reasonably calculate cliff-top deposition of boulders by tsunami and storm waves.

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More information

e-pub ahead of print date: 7 June 2019
Published date: 1 December 2019
Additional Information: Publisher Copyright: © 2019 John Wiley & Sons, Ltd.
Keywords: boulder transport model, cliff-top deposition, identification of tsunami or storm boulder, numerical simulation, wave-tank experiment

Identifiers

Local EPrints ID: 494629
URI: http://eprints.soton.ac.uk/id/eprint/494629
ISSN: 0197-9337
PURE UUID: 9125137e-1a94-4c9e-889d-40635e453464
ORCID for Masashi Watanabe: ORCID iD orcid.org/0000-0003-3670-7385

Catalogue record

Date deposited: 11 Oct 2024 16:49
Last modified: 12 Oct 2024 03:06

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Contributors

Author: Masashi Watanabe ORCID iD
Author: Kazuhisa Goto
Author: Fumihiko Imamura
Author: Andrew Kennedy
Author: Daisuke Sugawara
Author: Norihiro Nakamura
Author: Takayuki Tonosaki

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