Article : Shallow Water Turbulent Surface Wave Striking an Adverse Slope
Authors : Białecki, M.Institute of Geophysics, Polish Academy of Sciences, Warszawa, Poland, firstname.lastname@example.org, Bevis, M.School of Earth Sciences, Ohio State University, Columbus, Ohio, USA, email@example.com, Pan, E.Department of Civil Engineering, University of Akron, Akron, Ohio, USA, Zhou, H.School of Earth Sciences, Ohio State University, Columbus, Ohio, USA, Han, F.Department of Civil Engineering, University of Akron, Akron, Ohio, USA, Zhu, R.Department of Civil Engineering, University of Akron, Akron, Ohio, USA, Sun, Q.School of Resources and Geosciences, China University of Mining and Technology, Xuzhou, China, firstname.lastname@example.org, Xue, L.Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China, Zhu, S.School of Resources and Geosciences, China University of Mining and Technology, Xuzhou, China, Hekmatian, M. E.Faculty of Basic Sciences of Science and Research Branch, Islamic Azad University, Tehran, Iran; Nuclear Fuel Cycle Research School of Nuclear Science and Technology Research Institute (NSTRI), Tehran, Iran, email@example.com, Ardestani, V. E.Institute of Geophysics, University of Tehran, Tehran, Iran, firstname.lastname@example.org, Riahi, M. A.Institute of Geophysics, University of Tehran, Tehran, Iran, email@example.com, Bagh, A. M. K.Nuclear Fuel Cycle Research School of Nuclear Science and Technology Research Institute (NSTRI), Tehran, Iran; Faculty of Engineering of South Tehran Branch, Islamic Azad University, Tehran, Iran, firstname.lastname@example.org, Amini, J.Faculty of Engineering, University of Tehran, Tehran, Iran, email@example.com, Cheng, B.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu, China / Key Laboratory of Earth Exploration and Information Technology of Ministry of Education, Chengdu University of Technology, Chengdu, China / Meteorological Information and Signal Processing / Key Laboratory of Sichuan Higher Education Institutes, Chengdu University of Information Technology, Chengdu, China, firstname.lastname@example.org, Xu, T.3rd Geophysical Institute, Exploration and Production Institute, Southwest Oil and Gas Company, SINOPEC, Chengdu, China, Robbins, B.Fugro Aperio, Fugro Onshore Geotechnics, Wallingford, Oxfordshire, UK, Shen, Z. M.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu, China, Toushmalani, R.Department of Computer, Faculty of Engineering, Kangavar Branch, Islamic Azad University, Kangavar, Iran, email@example.com, Saibi, H.Laboratory of Exploration Geophysics, Department of Earth Resources Engineering, Faculty of Engineering, Kyushu University, Fukuoka, Japan, firstname.lastname@example.org, Chakravarthini, V.Centre for Earth and Space Sciences, University of Hyderabad, Hyderabad, India, email@example.com, Ramamma, B.Centre for Earth and Space Sciences, University of Hyderabad, Hyderabad, India, firstname.lastname@example.org, Białoń, W.Institute of Geophysics, Polish Academy of Sciences, Warszawa, Poland, email@example.com, Zarzycka, E.Institute of Geophysics, Polish Academy of Sciences, Warszawa, Poland, firstname.lastname@example.org, Lasocki, S.Institute of Geophysics, Polish Academy of Sciences, Warszawa, Poland, email@example.com, Bose, S. K.S.N. Bose National Centre for Basic Sciences, Kolkata 700064, India, firstname.lastname@example.org,
Abstract : The problem of a sinusoidal wave crest striking an adverse slope due to gradual elevation of the bed is relevant for coastal sea waves. Turbulence based RANS equations are used here under turbulence closure assumptions. Depth-averaging the equations of continuity and momentum, yield two differential equations for the surface elevation and the average forward velocity. After nondimensionalization, the two equations are converted in terms of elevation over the inclined bed and the discharge, where the latter is a function of the former satisfying a first order differential equation, while the elevation is given by a first order evolution equation which is treated by Lax-Wendroff discretization. Starting initially with a single sinusoidal crest, it is shown that as time progresses, the crest leans forwards, causing a jump in the crest upfront resulting in its roll over as a jet. Three cases show that jump becomes more prominent with increasing bed inclination.
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Qute : Białecki, M. ,Bevis, M. ,Pan, E. ,Zhou, H. ,Han, F. ,Zhu, R. ,Sun, Q. ,Xue, L. ,Zhu, S. ,Hekmatian, M. E. ,Ardestani, V. E. ,Riahi, M. A. ,Bagh, A. M. K. ,Amini, J. ,Cheng, B. ,Xu, T. ,Robbins, B. ,Shen, Z. M. ,Toushmalani, R. ,Saibi, H. ,Chakravarthini, V. ,Ramamma, B. ,Białoń, W. ,Zarzycka, E. ,Lasocki, S. ,Bose, S. K. ,Bose, S. K. , Shallow Water Turbulent Surface Wave Striking an Adverse Slope. Acta Geophysica Vol. 63, no. 4/2015