Characterizing interactive compound flood drivers in the Pearl River Estuary: A case study of Typhoon Hato (2017)

被引:1
|
作者
Lin, Qianru [1 ]
Shi, Luming [1 ]
Liang, Bingchen [1 ,2 ]
Wu, Guoxiang [1 ,2 ]
Wang, Zhenlu [1 ,2 ]
Zhang, Xuecheng [1 ]
Wu, Yi [1 ]
机构
[1] Ocean Univ China, Coll Engn, 1299 Sansha Rd, Qingdao 266404, Peoples R China
[2] Ocean Univ China, Shandong Prov Key Lab Ocean Engn, 238 Songling Rd, Qingdao 266100, Peoples R China
基金
中国国家自然科学基金;
关键词
Compound flooding; Pearl River Estuary; Nonlinear interactions; WRF; Delft3D; HEC-RAS; STORM-SURGE; RISK; DEPENDENCE; DISCHARGE; RAINFALL; HAZARD; TIDES; CHINA;
D O I
10.1016/j.jhydrol.2024.132270
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Tropical cyclone (TC) induced compound floods involve dynamic interactions among astronomical tides, storm surges, precipitation, and associated river pulses. This study employs a one-way coupled WRF, Delft3D, and HECRAS model to investigate the impacts of oceanic, pluvial, and fluvial processes on compound flood dynamics during Typhoon Hato (2017) in the Pearl River Estuary (PRE), South China. Total water levels driven by different combinations of flood drivers are modeled and analyzed. Relative contributions of each type of flood driver are quantified and used to categorize flood zones. This study highlights the persistent impacts of storm surges and their nonlinear interactions with other flood drivers. They can modify both the timing and magnitude of maximum water levels, thereby distorting tidal signals and contributing to post-TC landfall water level peaks. Along coastal regions, water levels exhibit three successive peaks, predominantly driven by storm surge, rainfall, and the combined actions of both factors, respectively. In upstream regions and coastal areas sheltered from islands, a singular water level peak arises exclusively from rainfall-runoff processes. Moreover, nonlinear interactions between surge and rainfall-runoff have non-negligible impacts on the relative contribution of individual flood drivers, which underscores the necessity of considering both rainfall and storm surge in modeling compound flood water levels. During the flooding period, peak storm surge and the following peak rainfall resulted in a time-varying distribution of flood zones. Alternating feedback between compounded and oceandominant areas manifests in the midsections of the upper PRE. Maximum flooding depth, extent, and duration are mainly influenced by rainfall. Storm surges play a secondary role, causing intense but short-lived flooding in coastal regions. These findings aid in understanding the generation mechanism of compound floods and provide references for hazard mitigation strategies.
引用
收藏
页数:14
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