scholarly journals THE NUMERICAL SIMULATION OF STORM-SURGE AND COASTAL INUNDATION OF 2007 TYPHOON SEPAT

2011 ◽  
Vol 1 (32) ◽  
pp. 16
Author(s):  
Yu-Hsien Lin ◽  
Hwung-Hweng Hwung ◽  
Ming-Chung Fang ◽  
Ray-Yeng Yang

A comprehensive numerical model for simulating storm surge has been aimed at the middle-east Taiwan Strait, in which contains the Penghu Channel (PHC) and Changyun Rise (CYR). The simulation results can be used to understand the direct impact of storm surge on the interest area during typhoon invades. The case in this study is Typhoon SEPAT, which passed through central Taiwan in 2007. The transport characteristics through the Taiwan Strait under the influence of Typhoon SEPAT were analyzed using both field observations and numerical simulations during the typhoon period. The results show that storm surge did not respond to the southerly winds but the northerly winds, in contrast to the wind waves. According to the influence of dynamical forces on the storm surge in the Taiwan Strait, the atmospheric pressure gradient is found to be the dominant force of the coastal inundation during the typhoon event. By comparing with the numerical experiment, the Coriolis force is found to have a negative contribution to the storm surge generation in the Taiwan Strait.

2017 ◽  
Vol 146 ◽  
pp. 47-57 ◽  
Author(s):  
Xiaolong Yu ◽  
Weiran Pan ◽  
Xiangjing Zheng ◽  
Shenjie Zhou ◽  
Xiaoqin Tao

Water ◽  
2019 ◽  
Vol 11 (11) ◽  
pp. 2331
Author(s):  
Renhao Wu ◽  
Qinghua Yang ◽  
Di Tian ◽  
Bo Han ◽  
Shimei Wu ◽  
...  

The oceanic response of the Taiwan Strait (TWS) to Typhoon Nesat (2017) was investigated using a fully coupled atmosphere-ocean-wave model (COAWST) verified by observations. Ocean currents in the TWS changed drastically in response to significant wind variation during the typhoon. The response of ocean currents was characterised by a flow pattern generally consistent with the Ekman boundary layer theory, with north-eastward volume transport being significantly modified by the storm. Model results also reveal that the western TWS experienced the maximum generated storm surge, whereas the east side experienced only moderate storm surge. Heat budget analysis indicated that surface heat flux, vertical diffusion, and total advection all contributed to changes in water temperature in the upper 30 m with advection primarily affecting lower depths during the storm. Momentum balance analysis shows that along-shore volume acceleration was largely determined by a combined effect of surface wind stress and bottom stress. Cross-shore directional terms of pressure gradient and Coriolis acceleration were dominant throughout the model run, indicating that the effect of the storm on geostrophic balance was small. This work provides a detailed analysis of TWS water response to typhoon passage across the strait, which will aid in regional disaster management.


2020 ◽  
Vol 10 (20) ◽  
pp. 7382
Author(s):  
Li Zhang ◽  
Shaoping Shang ◽  
Feng Zhang ◽  
Yanshuang Xie

Typhoons Soudelor (2015) and Dujuan (2015) were two of the strongest storms to affect the Taiwan Strait in 2015. This study investigated the response of the waters on the western bank of the Taiwan Strait to the passage of Soudelor and Dujuan. This included an investigation of the resonant coupling between the tide and storm surge, typhoon wave variation caused by the storm tide, and wave-induced water level rise. Analyses conducted using numerical model simulations and observations from tidal stations and buoys, obtained during the passage of both Soudelor and Dujuan, revealed that resonant coupling between the astronomical tide and storm surge in the Taiwan Strait was prominent, which resulted in tidal period oscillation on the storm surge and reduced tidal range. The tide wave arrived earlier than the predicted astronomical tide because of the existence of the storm surge, which was attributable to acceleration of the tidal wave caused by the water level rise. Wave height observations showed that the storm tide predominantly affected the waves, which resulted in wave heights that oscillated within the tidal period. Numerical experiments indicated that both the current and the water level affected wave height. Waves were affected mainly by the current in the middle of the Taiwan Strait, but mostly by water level when the water level was comparable with water depth. Wave setup simulations revealed that wave setup also oscillated within the tidal period, and that local bathymetry was the most important influencing factor of wave setup distribution.


2017 ◽  
Vol 43 (3) ◽  
pp. 289-298 ◽  
Author(s):  
Min Xu ◽  
Xianyan Wang ◽  
Xing Miao ◽  
Fuxing Wu ◽  
Mu Ma ◽  
...  

2015 ◽  
Vol 109 ◽  
pp. 198-209 ◽  
Author(s):  
Haiqing Yu ◽  
Huaming Yu ◽  
Yang Ding ◽  
Lu Wang ◽  
Liang Kuang

2002 ◽  
Vol 83 (3) ◽  
pp. 457-471 ◽  
Author(s):  
D TANG ◽  
D KESTER ◽  
I NI ◽  
H KAWAMURA ◽  
H HONG

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