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dc.contributor.authorMarwan
dc.date.accessioned2012-06-21T05:32:49Z
dc.date.available2012-06-21T05:32:49Z
dc.date.issued2010-01
dc.identifier.citationAndonowati and E. van Groesen, 2003, Optical pulse deforma-tion in second order non-linear media, Journal of Non-linear Optics Physics and Materials, vol. 12, no. 22. Andonowati, Marwan, E. van Groesen, 2003, Maximal Temporal Amplitude of generated wave group with two or three fre-quencies, Proc. of 2nd ICPMR&DT, Singapore, v2, 111-116. Andonowati, N. Karjanto, E. van Groesen, 2004, Extreme waves arising from downstream evolution of modulated wave dis-location and non-linear amplitude amplification for extreme fluid surface waves. Submitted to Mathematical Models and Methods in Applied Sciences. E. Cahyono, 2002, Analytical wave codes for predicting surface waves in a laboratory basin, Ph.D Thesis, Faculty of Mathe-matical Sciences Univ. of Twente,the Netherlands. M. A. Donelan and W. H. Hui, 1990, Mechanics of ocean surface waves. Surface Waves and Fluxes. Kluwer, Editors: G. L. Geernaert and W. J. Plants, 1:209-246. E. van Groesen, 1998, Wave groups in uni-directional surface wave models. Journal of Engineering Mathematics, 34: 215-226. E. van Groesen, Andonowati, E. Soewono, 1999, Non-linear effects in bi-chromatic surface waves. Proc. Estonian Acad. Sci., Mathematics and Physics, 48: 206-229. Longuet and M. S. Higgins, 1984, Statistical properties of wave groups in a random sea state. Philos. Trans. Roy. Soc. Lon-don, A312: 219-250. Marwan and Andonowati, 2003, Wave deformation on the propagation of bi-chromatics signal and its effect to the maxi-mum amplitude. JMS FMIPA ITB, vol. 8 no. 2: 81-87. O. M. Phillips, D. Gu and M. A. Donelan, 1993, Expected structure of extreme waves in a Gaussian sea. Part I. Theory and SWADE buoy measurements.J. Phys. Oceanogr, 23: 992-1000. C. T. Stansberg, 1998, On the non-linear behaviour of ocean wave groups. Ocean Wave Measurement and Analysis, Reston, VA, USA: American Society of Civil Engineers (ASCE), Editors: B. L. Edge and J. M. Hemsley, 2: 1227-1241. J. Westhuis, E. van Groesen, R. H. M. Huijsmans, 2000, Long time evolution of unstable bi-chromatic waves, Proc. 15th IWWW & FB, Caesarea Israel, 184-187. J. Westhuis, E. van Groesen, and R. H. M. Huijsmans, 2001, Experiments and numerics of bi-chromatic wave groups, J. Waterway, Port, Coastal and Ocean Engineering, 127: 334-342. G. B. Whitham, 1974, Linear and Non-linear Waves, John Wiley and Sons, New York.en_US
dc.identifier.issn1411-8904
dc.identifier.urihttp://hdl.handle.net/11617/1666
dc.description.abstractThis paper concerns with the down-stream propagation of waves over initially still water. Such study is relevant to generate waves of large amplitude in wave tanks of a hydrodynamic laboratory. Input in the form of a time signal is provided at the wave-maker located at one side of the wave tank; the resulting wave then propagates over initially still water towards the beach at the other side of the tank. Experiments show that nonlinear effects will deform the wave and may lead to large waves with wave heights larger than twice the original input; the deformations may show it as peaking and splitting. It is of direct scientific interest to understand and quantify the nonlinear distortion; it is also of much practical interest to know at which location in the wave tank, the extreme position, the waves will achieve their maximum amplitude and to know the amplitude amplification factor. To investigate this, a previously introduced concept called Maximal Temporal Amplitude (MTA) is used: at each location the maximum over time of the wave elevation. An explicit expression of the MTA cannot be found in general from the governing equations and generating signal. The model is used in this paper is a Korteweg-de Vries (KdV) model and third order approximation theory to calculate the approximate extreme positions for a class of wave. This class is the wave-groups that originate from initially bi-chromatics type of wave, described by superposition of two monochromatic waves. It is shown that, the extreme position depends on the amplitude and the wave length of the group. The theoretical results are verified with numerical as well as experimental results for comparison.en_US
dc.publisherlppmumsen_US
dc.subjectNonlinear distortionen_US
dc.subjectMaximal Temporal Amplitudeen_US
dc.subjectextreme positionen_US
dc.subjectbi- chromatics wavesen_US
dc.subjectKdV equationen_US
dc.subjectthird order approximationen_US
dc.titleON THE EXTREME POSITION OF PROPAGATION OF BICHROMATIC WAVE IN HYDRODYNAMIC LABORATORYen_US
dc.title.alternativePERAMBATAN GELOMBANG BICHROMATIC PADA POSISI EXTRIM DI LABORATORIUM HYDRODYNAMICen_US
dc.typeArticleen_US


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