Effect of the structural complexity of a coral reef on wave propagation: a case study from Komaka Island, Japan
The structural complexity of coral reefs has an essential impact on coastal wave propagation. Nevertheless, bathymetry data, from which complex structures of several meters in size can be ascertained, have yet to be used for numerical modelling. To investigate the effects of coral reef structural co...
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sg-ntu-dr.10356-1712232023-10-17T06:21:35Z Effect of the structural complexity of a coral reef on wave propagation: a case study from Komaka Island, Japan Watanabe, Masashi Kan, Hironobu Toguchi, Ken Nakashima, Yosuke Roeber, Volker Arikawa, Taro Earth Observatory of Singapore Social sciences::Geography Bottom Friction Coral Reefs The structural complexity of coral reefs has an essential impact on coastal wave propagation. Nevertheless, bathymetry data, from which complex structures of several meters in size can be ascertained, have yet to be used for numerical modelling. To investigate the effects of coral reef structural complexity on coastal wave propagation, we first obtained 1-m resolution bathymetry data from a multibeam echosounder on Komaka Island, Japan. Then we conducted numerical simulations of storm waves over the obtained bathymetry. The simulation results using fine topographic resolution demonstrate that vorticity over the reef slope is significant due to the structural complexity of coral reefs, including spurs and grooves. This implies that complex features of several meters over the reef slope induce wave-driven currents, which is often a pathway for nutrient transport. However, the calculated wave energy densities over the reef flat are mostly the same, even when coarse bathymetry resolution is used. Thus, the overall reef slope, edge, and flat account for most of the dissipation process of storm waves, whereas complex structures of several meters in size have little impact. In contrast, the coral structures several meters in size contribute to the ecosystem by facilitating seawater rather than dissipating extreme waves. This research was supported by a Grant-in-Aid for Scientific Research from the Japan Society for the Promotion of Science (Project Number JP16H06309; 21H04379; 22K14455). A Sasakawa Scientific Research Grant from the Japan Science Society supported this work. Volker Roeber acknowledges financial support from the I-SITE program Energy & Environment Solutions (E2S), the Communaut´e d’Agglom´eration Pays Basque (CAPB), and the Communaut´e R´egion Nouvelle Aquitaine (CRNA) for the chair position HPC-Waves. 2023-10-17T06:21:34Z 2023-10-17T06:21:34Z 2023 Journal Article Watanabe, M., Kan, H., Toguchi, K., Nakashima, Y., Roeber, V. & Arikawa, T. (2023). Effect of the structural complexity of a coral reef on wave propagation: a case study from Komaka Island, Japan. Ocean Engineering, 287, 115632-. https://dx.doi.org/10.1016/j.oceaneng.2023.115632 0029-8018 https://hdl.handle.net/10356/171223 10.1016/j.oceaneng.2023.115632 2-s2.0-85171588730 287 115632 en Ocean Engineering © 2023 Elsevier Ltd. All rights reserved. |
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Social sciences::Geography Bottom Friction Coral Reefs Watanabe, Masashi Kan, Hironobu Toguchi, Ken Nakashima, Yosuke Roeber, Volker Arikawa, Taro Effect of the structural complexity of a coral reef on wave propagation: a case study from Komaka Island, Japan |
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The structural complexity of coral reefs has an essential impact on coastal wave propagation. Nevertheless, bathymetry data, from which complex structures of several meters in size can be ascertained, have yet to be used for numerical modelling. To investigate the effects of coral reef structural complexity on coastal wave propagation, we first obtained 1-m resolution bathymetry data from a multibeam echosounder on Komaka Island, Japan. Then we conducted numerical simulations of storm waves over the obtained bathymetry. The simulation results using fine topographic resolution demonstrate that vorticity over the reef slope is significant due to the structural complexity of coral reefs, including spurs and grooves. This implies that complex features of several meters over the reef slope induce wave-driven currents, which is often a pathway for nutrient transport. However, the calculated wave energy densities over the reef flat are mostly the same, even when coarse bathymetry resolution is used. Thus, the overall reef slope, edge, and flat account for most of the dissipation process of storm waves, whereas complex structures of several meters in size have little impact. In contrast, the coral structures several meters in size contribute to the ecosystem by facilitating seawater rather than dissipating extreme waves. |
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Earth Observatory of Singapore |
author_facet |
Earth Observatory of Singapore Watanabe, Masashi Kan, Hironobu Toguchi, Ken Nakashima, Yosuke Roeber, Volker Arikawa, Taro |
format |
Article |
author |
Watanabe, Masashi Kan, Hironobu Toguchi, Ken Nakashima, Yosuke Roeber, Volker Arikawa, Taro |
author_sort |
Watanabe, Masashi |
title |
Effect of the structural complexity of a coral reef on wave propagation: a case study from Komaka Island, Japan |
title_short |
Effect of the structural complexity of a coral reef on wave propagation: a case study from Komaka Island, Japan |
title_full |
Effect of the structural complexity of a coral reef on wave propagation: a case study from Komaka Island, Japan |
title_fullStr |
Effect of the structural complexity of a coral reef on wave propagation: a case study from Komaka Island, Japan |
title_full_unstemmed |
Effect of the structural complexity of a coral reef on wave propagation: a case study from Komaka Island, Japan |
title_sort |
effect of the structural complexity of a coral reef on wave propagation: a case study from komaka island, japan |
publishDate |
2023 |
url |
https://hdl.handle.net/10356/171223 |
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1781793735796850688 |