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 language | English |
|---|---|
| Pages (from-to) | 2475-2504 |
| Number of pages | 30 |
| Journal | Natural Hazards and Earth System Sciences |
| Volume | 23 |
| Issue number | 7 |
| Early online date | 13 Jul 2023 |
| DOIs | |
| Publication status | Published - 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)).
| Funders | Funder number |
|---|---|
| NAFOSTED-RCUK | |
| National Foundation for Science and Technology Development | |
| Natural Environment Research Council | NE/S003150/1 |
| Natural Environment Research Council | |
| European Research Council | 884442 |
| European Research Council | |
| Nederlandse Organisatie voor Wetenschappelijk Onderzoek | 453-13-006 |
| Nederlandse Organisatie voor Wetenschappelijk Onderzoek | |
| Ministry of Science and Technology | DTDL-48/18 |
| Ministry of Science and Technology |