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Anna Lisa Cescon, James Andrew Graham Cooper and Derek W. T. Jackson
Beach ridges originate from various depositional processes and occur in a variety of settings. This paper assesses their nature and distribution on the islands of the Greater Caribbean based on a literature review and the identification of sites using Go...
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Jun Wang, Bo Yang, Bingchen Liang, Zai-Jin You, Zhenlu Wang and Zhaowei Wang
In this study, laboratory experiments were conducted to investigate the influence of changes in storm wave height and water level on beach response in a medium-scale wave flume. A schematic storm was simulated (rising, apex, and waning phases). A non-int...
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Marco Anzidei, Daniele Trippanera, Alessandro Bosman, Franco Foresta Martin, Fawzi Doumaz, Antonio Vecchio, Enrico Serpelloni, Tommaso Alberti, Sante Francesco Rende and Michele Greco
The island of Ustica (Italy) is constantly exposed to the effects of sea-level rise, which is threatening its coastal zone. With the aim of assessing the sea levels that are anticipated by 2150 CE under the climatic projections shown in the AR6 report fr...
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Zoran Kilibarda and Vesna Kilibarda
From 18 January 2013 (175.16 m a.s.l.) to 8 September 2020 (177.82 m a.s.l.), Lake Michigan experienced its fastest and highest rise (2.67 m) since 1860, when instrumental measurements began. Extensive foredunes developed since the last high lake levels ...
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Cyprien Bosserelle, Shari L. Gallop, Ivan D. Haigh and Charitha B. Pattiaratchi
Natural formations of rock and coral can support geologically controlled beaches, where the beach dynamics are significantly influenced by these structures. However, little is known about how alongshore variations in geological controls influence beach m...
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James A. Pollard, Elizabeth K. Christie, Susan M. Brooks and Tom Spencer
Gravel barriers represent physiographic, hydrographic, sedimentary, and ecological boundaries between inshore and open marine offshore environments, where they provide numerous important functions. The morphosedimentary features of gravel barriers (e.g.,...
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Laura Lemke and Jon K. Miller
Coastal erosion is controlled by two sets of factors, one related to storm intensity and the other related to a location?s vulnerability. This study investigated the role of each set in controlling dune erosion based on data compiled for eighteen histori...
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Sergey Agayan, Shamil Bogoutdinov, Roman Krasnoperov and Roman Sidorov
The article is focused on the approach based on the discrete mathematical analysis conception and continues a series of studies related to the application of the previously developed methodology to geophysical data analysis. The main idea of the study is...
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Gabriela Medellín, Martí Mayor, Christian M. Appendini, Ruth Cerezo-Mota and José A. Jiménez
Wave runup is a relevant parameter to determine the storm impact on barrier islands. Here, the role of the beach morphology on wave runup and storm impact was investigated at four coastal communities located on the northern Yucatan coast. Current wave co...
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Katerina Kombiadou, Susana Costas and Dano Roelvink
Short-term beach morphodynamics are typically modelled solely through storm-induced erosion, disregarding post-storm recovery. Yet, the full cycle of beach profile response is critical to simulating and understanding morphodynamics over longer temporal s...
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