2019
DOI: 10.1016/j.ecss.2019.106460
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Sensitivities of modelling storm surge to bottom friction, wind drag coefficient, and meteorological product in the East China Sea

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Cited by 34 publications
(20 citation statements)
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“…Astronomical tidal elevations on the open boundaries applied harmonics from the OTIS regional solution (Egbert and Erofeeva 2002). For the storm tide case, the proposed wind drag coefficients (Chu et al 2019) were used based on Zijlema et al (2012) adapted from Smith and Banke (1975).…”
Section: Storm Surge Modelmentioning
confidence: 99%
“…Astronomical tidal elevations on the open boundaries applied harmonics from the OTIS regional solution (Egbert and Erofeeva 2002). For the storm tide case, the proposed wind drag coefficients (Chu et al 2019) were used based on Zijlema et al (2012) adapted from Smith and Banke (1975).…”
Section: Storm Surge Modelmentioning
confidence: 99%
“…The best combination of the wind field and parameters can improve the performance of storm surge simulations. In addition, Chu et al (2019) also conclude that non-linear tide-surge effects contribute 37% at the time of peak surge.…”
Section: Major Topics In This Si Topic 1: Effects Of Typhoons On Wave Dynamicsmentioning
confidence: 83%
“…In another application of FVCOM, Chu et al (2019) investigate the sensitivities of the modeled storm surges to bottom friction, wind drag coefficient, and four meteorological products in the ECS. Based on model-to-data comparison during Typhoon Winnie (1997), it is found that the NCEP-CFSR wind field performs the best among the four wind field products (ERA-Interim, ERA5, CCMP, NCEP-CFSR).…”
Section: Major Topics In This Si Topic 1: Effects Of Typhoons On Wave Dynamicsmentioning
confidence: 99%
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“…Based on the previous study [26], the tropical cyclones influencing the SCC are roughly classified into four types: type 1 is a medium-turning tropical cyclone which propagates with a direction within 125 • E (Figure 1a); type 2 is similar to type 1, but with a propagation direction within a longitude range of 125 • E to 140 • E (Figure 1b); type 3 is a tropical cyclone that lands in Fujian province or dissipates in the Taiwan Strait (Figure 1c); type 4 is the one that lands in Zhejiang province, Jiangsu province, or disappears in the offshore (Figure 1d). Storm surge models have been developed along the SCC, and they mainly concentrated on studying a typhoon-induced storm surge process [23,27,28]. Although this region is vulnerable to storm surges, there has been little open literature reporting on the synergistic effects of key parameters in the wind and pressure field (forward speed, RMW, inflow angle, and central pressure), typhoon path, wind intensity, and topography on the modeling of storm surge and surge asymmetry along the SCC, which motivated this paper.…”
Section: Introductionmentioning
confidence: 99%