Is the tropical cyclone surge in Shanghai more sensitive to landfall location or intensity change?

Journal Article (2021)
Authors

Shuai Wang (Imperial College London)

Ralf Toumi (Imperial College London)

Q. Ye (Deltares, TU Delft - Coastal Engineering)

Q. Ke (TU Delft - Hydraulic Structures and Flood Risk)

Jeremy Bricker (University of Michigan, TU Delft - Hydraulic Structures and Flood Risk)

Zhan Tian (Southern University of Science and Technology )

Laixiang Sun (SOAS University of London, University of Maryland)

Research Group
Coastal Engineering
Copyright
© 2021 Shuai Wang, Ralf Toumi, Qinghua Ye, Q. Ke, J.D. Bricker, Zhan Tian, Laixiang Sun
To reference this document use:
https://doi.org/10.1002/asl.1058
More Info
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Publication Year
2021
Language
English
Copyright
© 2021 Shuai Wang, Ralf Toumi, Qinghua Ye, Q. Ke, J.D. Bricker, Zhan Tian, Laixiang Sun
Research Group
Coastal Engineering
Issue number
10
Volume number
22
Pages (from-to)
1-8
DOI:
https://doi.org/10.1002/asl.1058
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Abstract

It has been shown that the proportion of intense tropical cyclones (TCs) has been increasing together with a poleward migration of TC track. However, their relative importance to TC surge at landfall remains unknown. Here we examine the sensitivity of TC surge in Shanghai to landfall location and intensity with a new dynamical modelling framework. We find a surge sensitivity of 0.8 m (°N)−1 to landfall location, and 0.1 m (m s−1)−1 to wind speed in Shanghai during landfall. The landfall location and intensity are comparably important to surge variation. However, based on a plausible range of reported trends of TC poleward migration and intensity, the potential surge hazard due to poleward migration is estimated to be about three times larger than that by intensity change. The long-term surge risk in Shanghai is therefore substantially more sensitive to changes of TC track and landfall location than intensity. This may also be true elsewhere and in the future.