Temat: wave run-up - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Calculation of Wave Run-up Height in South Baltic Sea: Case Study at Coastal Research Station at Lubiatowo, Poland
Autorzy:: Morawski, M.
Różyński, G.
Szmytkiewicz, P.
Powiązania:: https://bibliotekanauki.pl/articles/241434.pdf
Data publikacji:: 2018
Wydawca:: Polska Akademia Nauk. Instytut Budownictwa Wodnego PAN
Tematy:: wave run-up
statistics
dissipative beach
Baltic Sea
Opis:: The paper presents recent investigations of beach run-up phenomena at the Coastal Research Station of the Institute of Hydro-Engineering of the Polish Academy of Sciences at Lubiatowo, Poland. The local beach is typical of open-sea coasts of the south Baltic Sea, featuring multiple longshore bars that form predominantly dissipative systems. Measurements were taken to verify the existing formulas for the run-up height, bearing in mind that they had been derived for entirely different, oceanic conditions. The results indicate that these formulations can be adapted to south Baltic Sea conditions. This however, will require significantly larger data sets, which we intend to obtain in the near future.
Źródło:: Archives of Hydro-Engineering and Environmental Mechanics; 2018, 65, 3; 203-291
1231-3726
Pojawia się w:: Archives of Hydro-Engineering and Environmental Mechanics
Dostawca treści:: Biblioteka Nauki

Artykuł

Skocz do pozycji: 2.

Tytuł:: Run-Up of Linear Long Waves on Uniform Slope in Lagrangian Description
Autorzy:: Chybicki, W.
Powiązania:: https://bibliotekanauki.pl/articles/241448.pdf
Data publikacji:: 2006
Wydawca:: Polska Akademia Nauk. Instytut Budownictwa Wodnego PAN
Tematy:: wave run-up
Langrangian description
Hamilton principle
hypergeometric functions
Opis:: The case of linear, two-dimensional long waves on a uniform slope is considered. It is assumed that the fluid is nonviscous and incompressible. In the present paper the description of the long wave proposed by Wilde (Wilde, Chybicki 2004) is based on the fundamental assumption that the vertical material lines of fluid remain vertical during the entire motion. The equations of motion are derived with the help of a variational formulation of the problem. The Lagrangian is the difference between the kinetic and potential energy of the fluid. In the paper a correction followed from dispersion to the results obtained by Shuto is presented.
Źródło:: Archives of Hydro-Engineering and Environmental Mechanics; 2006, 53, 2; 97-104
1231-3726
Pojawia się w:: Archives of Hydro-Engineering and Environmental Mechanics
Dostawca treści:: Biblioteka Nauki

Artykuł

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