Waves and Flows in Basins of Complex Geometry

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Oceans and Coastal Zones".

Deadline for manuscript submissions: closed (31 December 2022) | Viewed by 2544

Special Issue Editors


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Guest Editor
Department of Applied Mathematics, Nizhny Novgorod State Technical University, Minina St, 24, Nizhny Novgorod, Russia
Interests: natural and anthropogenic disasters; internal, edge and surface waves; physics of sea ice; wave climate; dynamics of pollutions; hydraulic engineering and constructions; numerical simulations; computational fluid dynamics
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Guest Editor
Ishlinsky Institute for Problems in Mechanics Russian Academy of Sciences, Prospekt Vernadskogo, 101-1, Moscow, Russia
Interests: mathematical modelling; mathematical physics; asymptotics methods; fluid dynamics

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Guest Editor
Institute of Marine Geology and Geophysics Far Eastern Branch Russian Academy of Sciences, Nauki St., 1B, Yuzhno-Sakhalinsk, Russia
Interests: infragravity waves; wind waves; swell; harbor oscillations; sea ice; chaotic vibrations

Special Issue Information

Dear Colleagues,

Dynamic processes in real water basins (e.g., marine areas, bays, fjords, straits, lakes and reservoirs) include waves of various types and wave-induced flows, gravity currents, convective, advective and diffusion processes, etc. All these processes are, generally speaking, nonlinear and can interact with each other. At the same time, natural basins have a complex bathymetry and an indented coastline, which significantly complicates research for practical problems. The origins for the occurrence of wave motions are various: fluctuations in atmospheric pressure and wind, tides and inertial movements, earthquakes and landslide processes, flow around bottom irregularities and anthropogenic causes. Waves and currents play an important role in the transformation of the sea bottom and coastline, changes in biolandscape, mixing of water layers, transport of pollutants and admixtures, propagation of acoustic signals and migration of marine animals, and can also be dangerous for marine engineering structures, surface and underwater navigation, etc.

This Special Issue is devoted to the description of nonlinear dynamics of wave fields (surface, internal, trapped, inertial and others) in horizontally and/or vertically inhomogeneous basins with boundaries having complex geometry. Inhomogeneity can be due to both a variable bottom depth and/or a vertical stratification in density and/or current, which can also be horizontally variable. In fact, this wide class of problems implies the mathematical modeling of the initial-boundary problem for the system of hydrodynamics equations for a horizontally and vertically inhomogeneous fluid (or approximate models of various complexity levels) in a domain of a geometrically complex configuration in the field of gravity and Coriolis forces, taking into account external conditions (tidal currents, various types of boundary conditions, atmospheric forcing, etc.).

We invite contributions covering a broad range of topics, including observational data and their analysis, theoretical estimates, numerical modeling, nonlinear fluid dynamics, wave interactions, Lagrangian transport and accounting the influence of additional factors (rotation, dissipation, tides, presence of waveguides, resonant properties of the water basin, etc.) in the context of wave phenomena in inhomogeneous environments.

Prof. Dr. Andrey Kurkin
Prof. Dr. Vitaly V. Bulatov
Dr. Dmitry Kovalev
Guest Editors

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Keywords

  • inhomogeneous basins
  • numerical modeling
  • fluid dynamics
  • observations
  • internal, surface, trapped and inertial waves
  • stratified flows
  • wave-induced currents
  • seiches
  • resonant oscillations
  • dynamics of surfactants, admixtures and sediments

Published Papers (1 paper)

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Research

27 pages, 21124 KiB  
Article
Analysis of Internal Solitary Waves in the Gulf of Oman and Sources Responsible for Their Generation
by Kamran Koohestani, Yury Stepanyants and Mohammad Nabi Allahdadi
Water 2023, 15(4), 746; https://doi.org/10.3390/w15040746 - 13 Feb 2023
Cited by 6 | Viewed by 1970
Abstract
A combination of multiple data sources has been used to study the characteristics of internal solitary waves (ISWs) in the Gulf of Oman (GoO). Water column stratification in the Gulf has been examined using field observations and World Ocean Atlas 2018 datasets. The [...] Read more.
A combination of multiple data sources has been used to study the characteristics of internal solitary waves (ISWs) in the Gulf of Oman (GoO). Water column stratification in the Gulf has been examined using field observations and World Ocean Atlas 2018 datasets. The spatiotemporal distribution of ISWs has been obtained from satellite images obtained by means of Synthetic Aperture Radar (SAR) and optical sensors taken from 2018 to 2020. The mechanisms of ISW generation in the GoO have been studied using the data revealed from different available sources. The results show that there are annually two major typical stratifications in the GoO throughout the year, strong stratification in May through September and weak stratification during other months. Dispersion relations corresponding to these types of stratification have been obtained with acceptable accuracy for both deep and shallow regions. The spatiotemporal distribution of ISWs demonstrates that the western and southern regions of the GoO are the hotspots for generation of ISWs in this basin. Several mechanisms of ISW generation in the GoO are discussed including tide, eddies, lee waves, and atmospheric perturbation; the latter one is, apparently, responsible for the appearance of large-amplitude ISWs. Full article
(This article belongs to the Special Issue Waves and Flows in Basins of Complex Geometry)
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