Towards RANS Parameterization of Vertical Mixing by Langmuir Turbulence in Shallow Coastal Shelves
Langmuir turbulence in the upper ocean is generated by the interaction between the wind-driven shear current and the Stokes drift velocity induced by surface gravity waves. In homogenous (neutrally stratified) shallow water, the largest scales of Langmuir turbulence are characterized by full-depth L...
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Scholar Commons
2013
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Online Access: | http://scholarcommons.usf.edu/etd/4945 http://scholarcommons.usf.edu/cgi/viewcontent.cgi?article=6141&context=etd |