A Comparative Study of Typhoon Hato (2017) and Typhoon Mangkhut (2018)—Their Impacts on Coastal Inundation in Macau

Author:

Yang Jie123,Li Linlin345,Zhao Kuifeng3,Wang Peitao6,Wang Dong3,Sou In Mei3,Yang Zhengtong3,Hu Jie3,Tang Xiaochun37,Mok Kai Meng8,Liu Philip Li‐Fan3910

Affiliation:

1. Key Laboratory of Coastal Disaster and Defence (Hohai University), Ministry of Education Hohai University Nanjing China

2. College of Harbor, Coastal and Offshore Engineering Hohai University Nanjing China

3. Department of Civil and Environmental Engineering National University of Singapore Singapore

4. Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, School of Earth Sciences and Engineering Sun Yat‐Sen University Guangzhou China

5. Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) Zhuhai China

6. National Marine Environmental Forecasting Center Beijing China

7. State Key Laboratory of Hydraulics and Mountain River Engineering Sichuan University Chengdu China

8. Department of Civil and Environmental Engineering University of Macau Macau China

9. School of Civil and Environmental Engineering Cornell University Ithaca NY USA

10. Institute of Hydrological and Ocean Research National Central University Taoyuan City Taiwan

Funder

National Natural Science Foundation of China

National Basic Research Program of China

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Reference74 articles.

1. Battjes J. A.(1974).Computation of set‐up longshore currents run‐up and overtopping due to wind‐generated waves((Doctoral Thesis)). Technische Hogeschool Delft Delft Netherlands. Retrieved fromhttp://resolver.tudelft.nl/uuid:e126e043‐a858‐4e58‐b4c7‐8a7bc5be1a44

2. Coastal flooding in Scituate (MA): A FVCOM study of the 27 December 2010 nor'easter

3. A Review of People’s Behavior in and around Floodwater

4. A geospatial framework to estimate depth of scour under buildings due to storm surge in coastal areas

5. A Non-Dimensional Stationary Hurricane Wave Model

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