Relevant bibliographies by topics / Wave condition

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  1. Journal articles

Academic literature on the topic 'Wave condition'

Author: Grafiati
Published: 18 May 2024

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Journal articles on the topic "Wave condition"

1

Mori, Nobuhito, Hajime Mase, and Tomohiro Yasuda. "FREAK WAVE AND WEATHER CONDITION." Coastal Engineering Proceedings 1, no. 32 (2011): 70. http://dx.doi.org/10.9753/icce.v32.waves.70.

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The kurtosis of the surface elevation, Benjamin-Feir Index (BFI) and directional spread are measures of nonlinear four-wave interactions and freak waves. The dependence of kurtosis, BFI and directional spread under typhoon conditions are examined by numerical simulations. The BFI is significantly large in the fourth quadrant of the typhoon while the directional spread is small in the fourth quadrant. It was found that the potentially possible area of freak wave occurrence is the fourth quadrant of the typhoon rather than the other quadrants.
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2

Yu, Wen, Fenggang Wang, Jianguo Lin, and Dong Li. "Numerical Simulation of the Force Acting on the Riser by Two Internal Solitary Waves." Applied Sciences 12, no. 10 (2022): 4873. http://dx.doi.org/10.3390/app12104873.

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An internal wave is a typical dynamic process. As an internal wave, an internal solitary wave usually occurs between two layers of fluids with different densities. Compared with general internal waves, internal solitary waves have large amplitudes, fast propagation speeds, short-wave periods, and often have tremendous energy. The propagation causes strong convergence and divergence of seawater and generates a sudden strong current. Due to its various characteristics, the propagation of internal solitary waves can cause serious harm to offshore engineering structures. Therefore, studying the ef
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3

Tang, Haoyun, Huilong Ren, Hui Li, and Qi Zhong. "Experimental Investigation of Wave-Induced Hydroelastic Vibrations of Trimaran in Oblique Irregular Waves." Shock and Vibration 2016 (2016): 1–17. http://dx.doi.org/10.1155/2016/8794560.

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The irregular wave condition, especially the oblique irregular wave condition, is the actual circumstances when trimaran is sailing in sea. In order to identify the characteristic of the wave-induced hydroelastic vibration in irregular waves, as well as investigate the change of vibration in different oblique irregular wave conditions, trimaran model tests were conducted to measure vibrations, wave impact, and motion under different azimuth and wave height. The vibration on main hull, side hull, and cross-desk is measured and analyzed separately to observe the influence of irregular wave in di
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4

Stresswave Technology Ltd. "Stress wave condition monitoring." NDT & E International 23, no. 4 (1990): 240. http://dx.doi.org/10.1016/0963-8695(90)90978-r.

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Stresswave Technology Ltd. "Stress wave condition monitoring." NDT International 23, no. 4 (1990): 240. http://dx.doi.org/10.1016/0308-9126(90)91714-5.

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6

Ismail, Mohd Arif, Nik Mohd Ridzuan Shaharuddin, Omar Yaakob, et al. "WAKE WASH OF A FAST SMALL BOAT IN RESTRICTED WATERS: MODEL TESTS AND FULL-SCALE MEASUREMENTS." Brodogradnja 73, no. 2 (2022): 93–119. http://dx.doi.org/10.21278/brod73206.

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This paper presents the model testing of an 8.23m boat with hard chine planning hull generated waves at the Kilim recreational park. Wake is considered one of the main causes of riverbank erosion due to the energy carried by waves hitting the riverbank. Initially, ship particulars were measured from actual boats to generate a hull form using MAXSURF software. A lines plan was then generated to fabricate the model using fibreglass. Experiments were conducted in the National Hydraulic Research Institute of Malaysia (NAHRIM) at various speeds at a constant operating draft. The wave patterns gener
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7

Lamacz, A., and B. Schweizer. "Outgoing wave conditions in photonic crystals and transmission properties at interfaces." ESAIM: Mathematical Modelling and Numerical Analysis 52, no. 5 (2018): 1913–45. http://dx.doi.org/10.1051/m2an/2018026.

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We analyze the propagation of waves in unbounded photonic crystals. Waves are described by a Helmholtz equation with x-dependent coefficients, the scattering problem must be completed with a radiation condition at infinity. We develop an outgoing wave condition with the help of a Bloch wave expansion. Our radiation condition admits a uniqueness result, formulated in terms of the Bloch measure of solutions. We use the new radiation condition to analyze the transmission problem where, at fixed frequency, a wave hits the interface between free space and a photonic crystal. We show that the vertic
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8

Randall, C. J. "Absorbing boundary condition for the elastic wave equation." GEOPHYSICS 53, no. 5 (1988): 611–24. http://dx.doi.org/10.1190/1.1442496.

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Extant absorbing boundary conditions for the elastic wave equation are generally effective only for waves nearly normally incident upon the boundary. High reflectivity is exhibited for waves traveling obliquely to the boundary. In this paper, a new and efficient absorbing boundary condition for two‐dimensional and three‐dimensional finite‐difference calculations of elastic wave propagation is presented. Compressional and shear components of the incident vector displacement fields are separated by calculating intermediary scalar potentials, allowing the use of Lindman’s boundary condition for s
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9

Taniguchi, Kenji. "Variations in Winter Ocean Wave Climate in the Japan Sea under the Global Warming Condition." Journal of Marine Science and Engineering 7, no. 5 (2019): 150. http://dx.doi.org/10.3390/jmse7050150.

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Future variations in the ocean wave climate caused by global warming could affect various coastal issues. Using a third-generation wave model, this study produced projections of the ocean wave climate for winter around Japan, focusing on the Japan Sea side. Wave simulation forcing (sea surface wind) was generated through five different global warming experiments. More than half the future wave projections showed an increasing tendency of the climatological mean significant wave height during winter. However, the maximum significant wave height did not show any clear tendency in future variatio
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10

Shin, Changsoo. "Sponge boundary condition for frequency‐domain modeling." GEOPHYSICS 60, no. 6 (1995): 1870–74. http://dx.doi.org/10.1190/1.1443918.

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Several techniques have been developed to get rid of edge reflections from artificial boundaries. One of them is to use paraxial approximations of the scalar and elastic wave equations. The other is to attenuate the seismic waves inside the artificial boundary by a gradual reduction of amplitudes. These techniques have been successfully applied to minimize unwanted seismic waves for time‐domain seismic modeling. Unlike time‐domain seismic modeling, suppression of edge reflections from artificial boundaries has not been successful in frequency‐domain seismic modeling. Rayleigh waves caused by c
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