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Titlebook: Computer Modelling of Seas and Coastal Regions; P. W. Partridge Book 1992 Computational Mechanics Publications 1992 environment.evolution.

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發(fā)表于 2025-3-23 11:14:40 | 只看該作者
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發(fā)表于 2025-3-23 14:29:03 | 只看該作者
https://doi.org/10.1007/978-981-15-7281-4e movement of floating pollutants and is also of paramount importance when evaluating the boundary conditions for the computation of coastal circulation; this paper presents an attempt to supplement the usual approach based on monochromatic waves or standard spectral simulations with an analysis of
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發(fā)表于 2025-3-23 18:29:52 | 只看該作者
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發(fā)表于 2025-3-24 02:07:44 | 只看該作者
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發(fā)表于 2025-3-24 05:27:45 | 只看該作者
https://doi.org/10.1007/978-981-15-7281-4on. It is important to estimate such energy loss when designing porous ocean structures, such as rubble-mound breakwaters in which the wave energy dissipation is usually the major goal. In this paper, the energy dissipation process is numerically modeled with the Boundary Integral Element Method (BI
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發(fā)表于 2025-3-24 09:56:26 | 只看該作者
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發(fā)表于 2025-3-24 19:36:16 | 只看該作者
Towards a Digitalised Sustainable Society,The average hourly wind speed values observed at the meteorological stations and extracted from the synoptic weather charts prepared periodically for weather forecasting are used to predict waves by the method of SMB (CERC [1]). Then, the Extreme Value Type I (Gumbel) distribution has been applied t
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發(fā)表于 2025-3-24 23:38:54 | 只看該作者
Fusion and Fission, Governors and Elevatorsy devised by Berkhoff (1972) and Schoenfeld (1972). This is the so-called mild slope equation and can be used only in case of gently bottomed or gradually-varied depths. So far several methods have been proposed to find out solutions to the aforementioned equation. The domain of the equation is the
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