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pro vyhledávání: '"Ken Melville"'
We consider the evolution of directional spectra of waves generated by constant and changing wind, modelling it by direct numerical simulation (DNS), based on the Zakharov equation. Results are compared with numerical simulations performed with the H
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b345bc9247f8d276d5dd71ff0b3b9675
https://doi.org/10.5194/egusphere-egu21-10435
https://doi.org/10.5194/egusphere-egu21-10435
Transformation of spectral shape during wind wave development and the transition from the spectrum of developing waves to the spectrum of fully developed waves are well documented in measurements, but have so far escaped all modelling, as well as the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1dd8fca98400f02880b22486e44ba1f8
https://doi.org/10.5194/egusphere-egu21-10437
https://doi.org/10.5194/egusphere-egu21-10437
Autor:
John A. Colosi, Falk Feddersen, C. Chris Chickadel, Sean Celona, Merrick C. Haller, James MacMahan, Amy F. Waterhouse, Tongtong Xu, Sean Haney, James A. Lerczak, Luc Lenain, John A. Barth, Ken Melville, Jennifer A. MacKinnon, P.B. Smit, Annika O'Dea
Publikováno v:
Eos. 100
In 2017, an ocean research team launched an unprecedented effort to understand what drives ocean currents in the overlap regions between surf zones and continental shelves.
Autor:
Ken Melville, Eric Terrill
Publikováno v:
The Journal of the Acoustical Society of America. 112:2401-2401
It is well understood that the presence of bubbles in the ocean can dramatically change the sound speed, attenuation, and scattering of underwater sound over a range of frequencies. Over the last few decades, rational theories have been developed and
Publikováno v:
The Journal of the Acoustical Society of America. 110:2668-2668
The properties of the turbulent boundary layer at the air–sea interface exhibits departures from classical wall bounded shear flows as a result of the free surface characterized by surface waves. As surface waves grow in the presence of wind, they
Conference
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