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dc.contributor.author Didenkulova I.I.
dc.contributor.author Pelinovsky E.N.
dc.contributor.author Kurkin A.A.
dc.contributor.author Zahibo N.
dc.contributor.author Levin B.V.
dc.contributor.author Soomere T.
dc.date.accessioned 2024-11-09T08:38:12Z
dc.date.available 2024-11-09T08:38:12Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13526362
dc.identifier.citation Doklady Earth Sciences, 2006, 411, 8, 1241-1243
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46413
dc.description.abstract The problem of runup of long nonbreaking waves on a plane slope is well developed from the mathematical point of view within the framework of nonlinear theory of shallow water, which allows for an analytical solution using the Carrier–Greenspan transform. Various examples of incident waves are considered in the literature. We also cite the latest publications. However, in all the papers cited, the incident wave was symmetric or antisymmetric with equal steepness of the leading and trailing slopes. As a result, the formulas for the runup height can be parameterized.
dc.title RUNUP OF NONLINEARLY DEFORMED WAVES ON A COAST
dc.type Статья
dc.identifier.doi 10.1134/S1028334X06080186


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