Rinse Wilmink, Robert McCall, Robbin Van Santen, Niels van Kuik, Stefan Pluis, Anouk de Bakker, Henk Steetzel
{"title":"XBEACH IMPLEMENTATION IN THE NEW NATIONAL COASTAL FLOOD RISK ASSESSMENT FRAMEWORK FOR THE DUTCH COAST","authors":"Rinse Wilmink, Robert McCall, Robbin Van Santen, Niels van Kuik, Stefan Pluis, Anouk de Bakker, Henk Steetzel","doi":"10.9753/icce.v37.management.46","DOIUrl":"https://doi.org/10.9753/icce.v37.management.46","url":null,"abstract":"Dunes and beaches protect large stretches of the Dutch coast against flooding from the sea. As prescribed by the Dutch Water Law, the Dutch dune coast is periodically assessed to ensure an acceptable level of flood risk in the hinterland. This safety assessment methodology is currently being renewed within the framework of the BOI program (Assessment and Design Instruments for flood defenses) to utilize the process-based storm impact model XBeach as replacement of the empirical dune erosion model DUROS+. The project consists of six steps: 1. XBeach model formulation improvements and model robustness, 2. XBeach calibration, 3. XBeach validation, 4. derivation of semi-probabilistic model input for the Dutch coast, 5. derivation of a failure definition and 6. implementing XBeach in a renewed flood risk assessment framework (Wilmink et al., 2020). The main goal of the project is to increase the accuracy of the flood risk assessment of dunes in the Netherlands by implementing XBeach as dune erosion model and develop a user-friendly GUI and guideline for the assessment framework.","PeriodicalId":497926,"journal":{"name":"Proceedings of ... Conference on Coastal Engineering","volume":"25 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135433771","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"PROPAGATION OF CARGO SHIP WAKE INTO SECONDARY CHANNELS","authors":"Alexandra Muscalus, Kevin Haas","doi":"10.9753/icce.v37.management.153","DOIUrl":"https://doi.org/10.9753/icce.v37.management.153","url":null,"abstract":"Cargo ship wake can be a strong and frequent source of energy along shorelines in the vicinity of commercial shipping channels. Large vessels in narrow channels produce low-frequency wake that consists of a positive front wave at the bow of the vessel, a depression (drawdown) spanning the length of the vessel, and an upwards surge produced by the stern wave at the stern. This low-frequency wake is followed by high-frequency wedge-shaped Kelvin wake, as well as continued low-frequency oscillations that may persist in the channel more than 30 minutes after a vessel passage. Low-frequency cargo ship wake with wave heights up to 2.8 meters was identified as the dominant source of erosion at Bird/Long Islands in the Savannah River, Georgia, USA based on the analysis of one month of Aquadopp measurements that captured over 300 large vessel wake events. The islands divide the river into the Main Channel, which contains the shipping channel, and the South Channel, a shallow, sheltered secondary channel trafficked only by small craft. Cargo ship wake was the primary energy source in both channels. The dominance of cargo ship wake energy in the sheltered South Channel demonstrated that the effects of wake extend beyond the shipping channel shorelines. This finding motivated three follow-up studies to quantify the extent and significance of cargo ship wake in the far-field, secondary channels connected directly or indirectly to the shipping channel.","PeriodicalId":497926,"journal":{"name":"Proceedings of ... Conference on Coastal Engineering","volume":"23 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135433775","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"WAVE TRANSMISSION AND DISSIPATION BY HYBRID (VEGETATED WITH MANGROVE) BREAKWATERS","authors":"José Partida, Edgar Mendoza","doi":"10.9753/icce.v37.structures.13","DOIUrl":"https://doi.org/10.9753/icce.v37.structures.13","url":null,"abstract":"In recent years a group of studies for coastal protection (Hashim and Catherine (2013), Maza et al. (2018), Tomiczek et al. (2020), among others) have been carried out to determine drag coefficients in mangrove forests due to ocean waves. Following the mangrove hybrid platform concept by Tagaki (2019), and actual projects such as the mangrove rehabilitation site in the Jakarta Fishing Port, the main objective of this study was to propose and test a hybrid structure capable of controlling wave energy via breaking and dissipation. The experimental tests focused on determining the rates of the wave energy distribution (reflection, transmission and dissipation) due to the presence of an afforested mangrove zone in the upper part of the breakwater. A fixed-bottom small-scale model was tested under normal and extreme marine regimes. The prototype dimensions of the breakwater are total height 5.70 m, crest width 10 m, seaside slope 2:1 (H:V) and leeward slope (1.5:1). The barrier is composed of a rigid bottom built of artificial elements (cubipods) and a long crown intended to be vegetated (with red mangroves, for example). The rationale behind this configuration is to provide ecosystem services by an artificially built mangrove forest protected by the rigid bottom. The experimental program consisted of 54 experiments divided into 7 groups corresponding to regular and irregular waves, mean and extreme and high and low tide conditions. Other variables of interest were the density and spatial distribution of mangroves, such as core materials.","PeriodicalId":497926,"journal":{"name":"Proceedings of ... Conference on Coastal Engineering","volume":"79 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135433937","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Christa van Ijzendoorn, Caroline Hallin, Sierd de Vries
{"title":"IMPLICATIONS OF SPATIAL GRAIN SIZE VARIABILITY FOR AEOLIAN TRANSPORT","authors":"Christa van Ijzendoorn, Caroline Hallin, Sierd de Vries","doi":"10.9753/icce.v37.sediment.49","DOIUrl":"https://doi.org/10.9753/icce.v37.sediment.49","url":null,"abstract":"Coastal dunes are crucial for coastal protection, habitat development and recreation. In recent years, their strength as a long-term building with nature approach has been explored in engineering projects. To improve implementation strategies, prediction of the development of the dune system is necessary. Aeolian sediment transport models may aid in informed design and decision-making. However, many aspects of aeolian sediment transport models need a thorough understanding to give reliable predictions. This research particularly focuses on grain size and assesses its effects on aeolian sediment transport at varying spatial and temporal scales. The aim is to provide recommendations on the relevance of spatial grain size variations in aeolian sediment transport modelling for coastal maintenance applications. For this purpose, we apply the aeolian sediment transport model AeoLiS, which allows for multi-fraction transport simulations (Hoonhout, 2017).","PeriodicalId":497926,"journal":{"name":"Proceedings of ... Conference on Coastal Engineering","volume":"8 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135433939","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Donatus Bapentire Angnuureng, Emmanuel Kwadwo Brempong, None Rafael Almar
{"title":"MULTI-PLATFORM MONITORING OF COASTAL EROSION AT A POCKET BEACH","authors":"Donatus Bapentire Angnuureng, Emmanuel Kwadwo Brempong, None Rafael Almar","doi":"10.9753/icce.v37.sediment.4","DOIUrl":"https://doi.org/10.9753/icce.v37.sediment.4","url":null,"abstract":"As in many other regions of the world, coastal recession in West and Central Africa is the result of natural factors, anthropogenic factors, or both (Anthony et al., 2016; Luijendijk et al., 2018), and when it occurs, it may continue unless it is firmly addressed. Erosion along Ghana's coastline is endemic as in most of the Gulf of Guinea countries in West Africa. The current challenge is how to document and understand the dimensions of erosion despite limited human and logistical capacity. Regular monitoring of coastal areas is a prerequisite to evade any imminent erosive disaster within the coastal cities (Angnuureng et al., 2022). Data-driven decisions have remained more uncertain because most monitoring platforms are unable to capture events of a certain frequency. The main goal of this work is to test the feasibility of using multiple sources of remote sensing platforms to assess the dynamics of a pocket beach at Elmina in Ghana, as a showcase for local governance.","PeriodicalId":497926,"journal":{"name":"Proceedings of ... Conference on Coastal Engineering","volume":"66 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135433994","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Maximilian Streicher, Yuri Pepi, Chiara Ricci, Leopoldo Franco, Giorgio Bellotti, Steven Hughes, Peter Troch
{"title":"WAVE OVERTOPPING OVER A DIKE FOR VARIABLE WATER LEVEL","authors":"Maximilian Streicher, Yuri Pepi, Chiara Ricci, Leopoldo Franco, Giorgio Bellotti, Steven Hughes, Peter Troch","doi":"10.9753/icce.v37.structures.46","DOIUrl":"https://doi.org/10.9753/icce.v37.structures.46","url":null,"abstract":"The still water level (SWL) during a storm is always dynamic (storm surge). The variability of the water level can be schematized as a time-varying hydrograph of a certain duration. The average wave overtopping discharge q is a function of the ratio between the freeboard Rc (the structure crest elevation above SWL) and the significant wave height Hm0. Since the variation during a storm of the SWL changes the freeboard Rc, the wave overtopping discharge is variable. Typically, in the laboratory the wave overtopping on coastal defense structures is investigated for a constant water level (CWL) and a pre‐determined structural exposure time frame. This exposure time frame is often representative for the storm surge peak or for a statistically representative number of individual waves (e.g. 1000 waves), not considering any variable water level (VWL). For the case of wave overtopping in VWL conditions, no validated prediction formulae exist (Kerpen et al. 2020) and the prediction is rather based on safe assumptions and engineering judgement. This research investigated the influence of a VWL on the prediction of the average wave overtopping discharge q.","PeriodicalId":497926,"journal":{"name":"Proceedings of ... Conference on Coastal Engineering","volume":"4 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135434019","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Carly Portch, Michael Cuttler, Mark Buckley, Jeff Hansen, Ryan Lowe
{"title":"HOW BEACH STATE INFLUENCES WAVE RUNUP ON A PERCHED BEACH IN SOUTHWESTERN AUSTRALIA","authors":"Carly Portch, Michael Cuttler, Mark Buckley, Jeff Hansen, Ryan Lowe","doi":"10.9753/icce.v37.currents.12","DOIUrl":"https://doi.org/10.9753/icce.v37.currents.12","url":null,"abstract":"Approximately 20 to 30 percent of the world’s coastlines are fronted by shallowly buried or outcropping shore platforms overlain by perched beaches (Kirk, 1977; Marshall and Stephenson, 2011; Trenhaile, 2002). Seasonal erosion of perched sediment can shift the beach state from ‘accreted’ to ‘exposed’ (Gallop et al., 2011), and the effect this has on wave-induced flood risk (known as wave runup) is unknown. As sea levels rise and storm severity increases, understanding how beach state influences wave runup is crucial for minimising coastal hazard risk and managing perched beach coastlines. In this work, idealised numerical modelling and field observations along a perched beach in southwestern Australia were used to quantify the influence of beach state on wave runup, setup, and swash processes.","PeriodicalId":497926,"journal":{"name":"Proceedings of ... Conference on Coastal Engineering","volume":"43 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135434020","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Miguel Esteban, Justin Valdez, Lau Jamero, Nicholson Tan, Ariel Rica, Paolo Valenzuela, Rex Ronter Ruiz, Brian Sumalinog, Glacer Vasquez, Christopher Chadwick, None Tomoya Shibayama
{"title":"SURVEY OF STORM SURGE DUE TO TYPHOON RAI IN DECEMBER 2021 IN THE PHILIPPINES","authors":"Miguel Esteban, Justin Valdez, Lau Jamero, Nicholson Tan, Ariel Rica, Paolo Valenzuela, Rex Ronter Ruiz, Brian Sumalinog, Glacer Vasquez, Christopher Chadwick, None Tomoya Shibayama","doi":"10.9753/icce.v37.management.15","DOIUrl":"https://doi.org/10.9753/icce.v37.management.15","url":null,"abstract":"Typhoon Rai, the last typhoon in the Western Pacific basin in 2021, entered the Philippine Area of Responsibility (PAR) on the 14th December at 23:00 Philippine Standard Time with a minimum central pressure of 985 hPa and maximum sustained winds of 100 km/h (NDRRMC 2022). The typhoon made its first of nine landfalls at Siargao Island in Surigao del Norte on the 16th December 2021 13:30 PST and continued to bring strong winds and rainfall to the Visayas region. The storm was one of the strongest typhoons to have hit the Philippines in recent times, and the government declared a State of Calamity across 493 cities and municipalities (NDRRMC 2022). The typhoon damaged more than 1.1 million houses in the Central Visayas region, and caused a total of 220 total reported deaths and 546 injuries. In the present work, the authors surveyed the storm surge heights in a variety of coastal areas of Cebu and Bohol islands.","PeriodicalId":497926,"journal":{"name":"Proceedings of ... Conference on Coastal Engineering","volume":"41 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135434025","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"STORM AND TSUNAMI OVERWASH SEDIMENT TRANSPORT INFERRED FROM RECENT DEPOSITS","authors":"Bruce Jaffe, SeanPaul La Selle","doi":"10.9753/icce.v37.sediment.65","DOIUrl":"https://doi.org/10.9753/icce.v37.sediment.65","url":null,"abstract":"Overwash deposits from storms and tsunamis record information about sediment transport and flow that can be used to inform hazard assessments. Here we explore deposits from two extreme wave events: (1) the 2012 Hurricane Sandy, a Category 5 hurricane that is the largest storm in the Atlantic basin on historical record, and (2) the 2011 Tohoku-oki tsunami, created by a 9.0 Mw earthquake, that was up to 20 m high at the coast.","PeriodicalId":497926,"journal":{"name":"Proceedings of ... Conference on Coastal Engineering","volume":"23 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135434095","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Mara M. Orescanin, Liliana Velasquez Montoya, John Plant, Cynthia Williamson, Collin Brennan
{"title":"MORPHODYNAMICS AT THE MOUTH OF A BAR-BUILT ESTUARY: CARMEL RIVER, CA, USA","authors":"Mara M. Orescanin, Liliana Velasquez Montoya, John Plant, Cynthia Williamson, Collin Brennan","doi":"10.9753/icce.v37.sediment.43","DOIUrl":"https://doi.org/10.9753/icce.v37.sediment.43","url":null,"abstract":"Bar-built estuaries (BBEs), also known as Intermittently Closed Estuaries (ICEs), are common to coastal climates with a strong seasonal precipitation pattern and waves including the US West Coast, Australia, South Africa, and Western Europe (McSweeney et al, 2017). In California, USA, these BBEs typically go through seasonal morphological transitions from a closed state to open state as precipitation increases during the winter months. However, timing of these events is challenging owing to variable behavior for given environmental forcing conditions, and as a result often lead to intermittent flooding of the surrounding areas that is difficult to predict (Behrens et al., 2013; Orescanin and Scooler, 2018). This study uses a compilation of observations using in-situ moorings, topographic beach surveys, and remote sensing from unmanned aerial systems (UAS) to assess rates of morphological change at the Carmel River, CA, USA.","PeriodicalId":497926,"journal":{"name":"Proceedings of ... Conference on Coastal Engineering","volume":"100 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135434103","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}