Tidal Asymmetry and Energy Variation Due to Sea-Level Rise in a Macro Tidal Bay

Suh, Seung-Won

doi:10.2112/si75-154.1

Cited by 3 publications

(1 citation statement)

References 12 publications

Supporting

Mentioning

Contrasting

Unclassified

Order By: Relevance

“…계절적 해수면 변화는 Amiruddin et al(2015), Cheng et al(2015), Cui and Zorita(1998), Dangendorf et al(2013), Kang et al(2008), Marcos et al (2012), Méndez et al(2006), Menéndez and Woodworth (2010), Pugh and Woodworth(2014), Watson(2015), Wijeratne et al(2008) 등의 연구에서 계절적 및 연간 변화를 지역적 또 는 전 세계적 측면으로 다룬 바 있다. 장기간 변화되는 해수 면은 발해만과 황해에 인위적인 연안 공사로부터 영향을 받 으며, 조석 비대칭에 변화를 줄 수 있다 (Pelling et al, 2013;김현정 • 서승원 Suh et al, 2014;Suh, 2016). 또한 18.6년 주기의 장주기 조석 변화에 따라 해수면에 장기간 영향을 미친다 (Baart et al, 2012;Cheng et al, 2016;Pugh and Woodworth, 2014;Watson, 2015).…”

Section: 서 론unclassified

Vulnerability Analyses of Wave Overtopping Inundation by Synthesized Typhoons with Sea-Level Rise

Kim¹,

Suh²

2019

J Korean Soc Coast Ocean Eng

View full text Add to dashboard Cite

Storm surges caused by a typhoon occur during the summer season, when the sea-level is higher than the annual average due to steric effect. In this study, we analyzed the sea-level pressure and tidal data collected in 1 h intervals at Incheon, Kunsan, Mokpo, Seogwipo stations on the Yellow Sea coast to analyze the summer season storm surge and wave overtopping. According to our analyses, the summer mean sea-level rise on the west and south coasts is approximately 20 cm and 15 to 20 cm higher than the annual mean sea-level rise. Changes in sea-level rise are closely related to changes in seasonal sea-level pressure, within the range of 1.58 to 1.73 cm/ hPa. These correlated mechanisms generates a phase difference of one month or more. The 18.6 year long period tidal constituents indicate that in 2090, the amplitude of the M 2 basin peaks on the southwest coast. Therefore, there is a need to analyze the target year for global warming and sea-level rise in 2090. Wave overtopping was simulated considering annual mean sea-level rise, summer sea level rise, the combined effect of nodal factor variation, and 100-year frequency storm surge. As a result, flooding by wave overtopping occurs in the area of Suyong Bay, Busan. In 2090, overtopping discharges are more than doubled than those in Marine City by the recent typhoon Chaba. Adequate coastal design is needed to prepare for flood vulnerability.

show abstract