Výsledky vyhledávání - "Martin, Calin I."

Akademický článek

A wave-breaking result for azimuthally varying water flows in cylindrical coordinates

Autor: Martin, Calin I.

Publikováno v: In Journal of Differential Equations 25 January 2025 416 Part 1:143-158

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Hamiltonian approach to modelling interfacial internal waves over variable bottom

Autor: Ivanov, Rossen I., Martin, Calin I., Todorov, Michail D.

Publikováno v: Physica D: Nonlinear Phenomena, Volume 433 (2022) 133190 (open access)

We study the effects of an uneven bottom on the internal wave propagation in the presence of stratification and underlying non-uniform currents. Thus, the presented models incorporate vorticity (wave-current interactions), geophysical effects (Coriol

Externí odkaz: http://arxiv.org/abs/2203.02590

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On rotational flows with discontinuous vorticity beneath steady water waves near stagnation

Autor: Chen, Lin, Basu, Biswajit, Martin, Calin-I

We numerically investigate the flow structure of periodic steady water waves of fixed relative mass flux propagating on rotational flows with piece-wise constant vorticity. We show that for wave solutions along the global bifurcation diagram the stag

Externí odkaz: http://arxiv.org/abs/2011.11775

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On the time-evolution of resonant triads in rotational capillary-gravity water waves

Autor: Ivanov, Rossen I., Martin, Calin I.

Publikováno v: Physics of Fluids 31 (2019) 117103

We investigate an effect of the resonant interaction in the case of one-directional propagation of capillary-gravity surface waves arising as the free surface of a rotational water flow. Specifically, we assume a constant vorticity in the body of the

Externí odkaz: http://arxiv.org/abs/1911.05213

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Surface waves over currents and uneven bottom

Autor: Compelli, Alan C., Ivanov, Rossen I., Martin, Calin I., Todorov, Michail D.

Publikováno v: Deep-Sea Research Part II 160 (2019) 25-31

The propagation of surface water waves interacting with a current and an uneven bottom is studied. Such a situation is typical for ocean waves where the winds generate currents in the top layer of the ocean. The role of the bottom topography is taken

Externí odkaz: http://arxiv.org/abs/1811.03140

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