Climate-induced storminess forces major increases in future storm surge hazard in the South China Sea region

Melissa Wood, Ivan D. Haigh*, Quan Quan Le, Hung Nghia Nguyen, Hoang Ba Tran, Stephen E. Darby, Robert Marsh, Nikolaos Skliris, Joël J.M. Hirschi, Robert J. Nicholls, Nadia Bloemendaal

*Corresponding author for this work

Research output: Contribution to JournalArticleAcademicpeer-review

Abstract

Coastal floods, driven by extreme sea levels, are one of the most dangerous natural hazards. The people at highest risk are those living in low-lying coastal areas exposed to tropical-cyclone-forced storm surges. Here we apply a novel modelling framework to estimate past and/or present and future storm-surge-level and extreme-sea-level probabilities along the coastlines of southern China, Vietnam, Cambodia, Thailand, and Malaysia. A regional hydrodynamic model is configured to simulate 10ĝ€¯000 years of synthetic tropical cyclone activity, representative of a past/present (1980-2017) and high-emission-scenario future (2015-2050) period. Results show that extreme storm surges, and therefore total water levels, will increase substantially in the coming decades, driven by an increase in the frequency of intense tropical cyclones. Storm surges along the southern Chinese and northern and southern Vietnamese coastlines increase by up to 1ĝ€¯m, significantly larger than expected changes in mean sea-level rise over the same period. The length of coastline that is presently exposed to storm surge levels of 2.5ĝ€¯m or greater will more than double by 2050. Sections of Cambodian, Thai, and Malaysian coastlines are projected to experience storm surges (at higher return periods) in the future, not previously seen, due to a southward shift in tropical cyclone tracks. Given these findings, coastal flood management and adaptation in these areas should be reviewed for their resilience against future extreme sea levels.

Original languageEnglish
Pages (from-to)2475-2504
Number of pages30
JournalNatural Hazards and Earth System Sciences
Volume23
Issue number7
Early online date13 Jul 2023
DOIs
Publication statusPublished - 2023

Bibliographical note

Funding Information:
This work was supported by the UK Natural Environment Research Council (grant no. NE/S003150/1) and, in Vietnam, by the National Foundation for Science and Technology Development (NAFOSTED-RCUK) fund and the Ministry of Science and Technology (Mekong River project, code DTDL-48/18). Nadia Bloemendaal was funded by a VICI grant from the Netherlands Organization for Scientific Research 569 (NWO grant no. 453-13-006) and the ERC Advanced Grant (COASTMOVE (grant no. 884442)).

Publisher Copyright:
© Copyright:

Funding

This work was supported by the UK Natural Environment Research Council (grant no. NE/S003150/1) and, in Vietnam, by the National Foundation for Science and Technology Development (NAFOSTED-RCUK) fund and the Ministry of Science and Technology (Mekong River project, code DTDL-48/18). Nadia Bloemendaal was funded by a VICI grant from the Netherlands Organization for Scientific Research 569 (NWO grant no. 453-13-006) and the ERC Advanced Grant (COASTMOVE (grant no. 884442)).

FundersFunder number
NAFOSTED-RCUK
National Foundation for Science and Technology Development
Natural Environment Research CouncilNE/S003150/1
Natural Environment Research Council
European Research Council884442
European Research Council
Nederlandse Organisatie voor Wetenschappelijk Onderzoek453-13-006
Nederlandse Organisatie voor Wetenschappelijk Onderzoek
Ministry of Science and TechnologyDTDL-48/18
Ministry of Science and Technology

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