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Alas, reading the entire article may require a subscription. click the envelope icon to have new results periodically delivered by email.Ībstracts are freely available for most of the articles.click "Sort by date" to show just the new additions, sorted by date.click "Since Year" to show only recently published papers, sorted by relevance.To find newer articles, try the following options in the left sidebar: Your search results are normally sorted by relevance, not by date. Finally, we formulate the sorting enforced by wave-height distributions during a storm, demonstrating how sorting is a direct manifestation of regional hydroclimatology.Get the most out of Google Scholar with some helpful tips on searches, email alerts, citation export, and more. Then, we obtain an expression for the longshore clast displacement under the fluid-induced pressure impulse of a given wave. Guided by these observations, we develop a new model quantifying the critical wave height for a certain clast mass mobilization. We utilize the unique setting of the Dead Sea shores where rapidly falling water levels allow isolating boulder transport during individual storms. Here, we use smart boulders equipped with loggers recording underwater, real-time, intra-storm clast motion, and measured longshore displacement of varied-mass marked boulders during storms. However, limited information on intra-storm clast motion restricts theory development for coastal gravel sorting and coastal management of longshore transport. This fundamental process is important under changing sea-levels and increased storm frequency and intensity. Storm waves transport and sort coarse gravel along coasts.
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