<i>Preface</i> Large amplitude internal waves in the coastal ocean

the pressure waves generated by fireworks, it seems contro- versial to raise the suspicion that pressure waves may possibly favor the appearance of traumatic cranial and

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In the bottom layer the fluid moves in the opposite direction of the internal wave propagation, but under the influence of the reverse flow, when the bulk of the velocity field of

The effect of the wind shear on the roll structures of nonlinear internal gravity waves (IGWs) in the Earth’s at- mosphere with the finite vertical temperature gradients is

Results are qualitatively consistent with the fluid model: the effective plasma frequency decreases, and the frequency range of the Alfvén branch is reduced when the temperature

As the harbour resonance is excited by the open sea waves, which are predominantly generated by the Proudman reso- nance, the next step is to explore atmosphere-ocean energy

through porous solid saturated with non-viscous fluid results in the three reflected waves and the four waves refracted to porous medium saturated with two immiscible viscous

Although the waves’ heights in the extreme regime are similar in magnitude to those found for Zone 01 (Alta Guajira), the extreme waves associated with the passage of cold fronts