Breaking and Dissipation of Ocean Surface Waves

By A. Babanin. 2011

216 citations recorded by the source corpus.

Subfields: Demography, Genetics, Political Science and International Relations

View Paper: https://www.semanticscholar.org/paper/6d11442e411cac961820d02a875b46062b0074aa

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Demography

1. J. Thomson
2. Arnaud Mussot
3. Frédéric Dias
4. John M. Dudley
5. Goëry Genty
6. A. Chabchoub

In Genetics

1. J. Thomson
2. Arnaud Mussot
3. Frédéric Dias
4. John M. Dudley
5. Goëry Genty
6. A. Chabchoub

In Political Science and International Relations

1. J. Thomson
2. Arnaud Mussot
3. Frédéric Dias
4. John M. Dudley
5. Goëry Genty
6. A. Chabchoub

Citations in the corpus

• Rogue waves and analogies in optics and oceanography (2019, methodology): “ is used in an NLSE context to describe the steepening of an optical envelope from nonlinear focussing [32], optical carrier waves themselves do not \break" or plunge as they do in hydrodynamics [33, 34]. There are also important dierences concerning measurements. Specically, experiments in opt”
• Wave Breaking Dissipation Observed with “SWIFT” Drifters (2012, background): “For some wave conditions, this limitation will be severe given the expectation that the depth-breaking turbulence scales with wave height (Babanin 2011) or water depth (Feddersen 2012).”
• User manual and system documentation of WAVEWATCH III R version 4.18 (2014, background): “Here, they are referred to as swell dissipation and parameterized in terms of the interaction of waves with oceanic turbulence (Babanin, 2011).”