Abstract
Sea-level rise, as a result of global warming, may lead to more natural disasters in coastal regions where there are substantial aggregations of population and property. Thus, this paper focuses on the impact of sea-level rise on the recurrence periods of extreme water levels fitted using the Pearson type III (P-III) model. Current extreme water levels are calculated using observational data, including astronomical high tides and storm surges, while future extreme water levels are determined by superposing scenario data of sea-level rise onto current extreme water levels. On the basis of a case study using data from Shandong Province, China, results indicated that sea-level rise would significantly shorten the recurrence periods of extreme water levels, especially under higher representative concentration pathway (RCP) scenarios. Results showed that by the middle of the century, 100-year current extreme water levels for all stations would translate into once in 15–30 years under RCP 2.6, and once in ten to 25 years under RCP 8.5. Most seriously, the currently low probability event of a 1000-year recurrence would become common, occurring nearly every 10 years by 2100, based on projections under RCP 8.5. Therefore, according to this study, corresponding risk to coastlines could well be increase in future, as the recurrence periods of extreme water levels would be shortened with climate change.
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Acknowledgments
Observational data from tide-gauge stations were provided by the National Marine Data and Information Service, People’s Republic of China. This work was supported by the National Science and Technology Support Program (Grant No. 2013BAK05B04), the National Natural Science Foundation of China (Grant No. 41530749) and the Clean Development Mechanism (CDM) Funding Projects of China (Grant No. 2013034). The authors would also like to thank Dr. Tao Pan, Dongsheng Zhao, and Yunhe Yin whose suggestions and comments greatly improved the final version of this paper.
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Wu, S., Feng, A., Gao, J. et al. Shortening the recurrence periods of extreme water levels under future sea-level rise. Stoch Environ Res Risk Assess 31, 2573–2584 (2017). https://doi.org/10.1007/s00477-016-1327-2
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DOI: https://doi.org/10.1007/s00477-016-1327-2