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contributor authorSmyth, W. D.
contributor authorCarpenter, J. R.
contributor authorLawrence, G. A.
date accessioned2017-06-09T17:18:34Z
date available2017-06-09T17:18:34Z
date copyright2007/06/01
date issued2007
identifier issn0022-3670
identifier otherams-82913.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4226080
description abstractDirect simulations are used to study turbulence and mixing in Holmboe waves. Previous results showing that mixing in Holmboe waves is comparable to that found in the better-known Kelvin?Helmholtz (KH) billows are extended to cover a range of stratification levels. Mixing efficiency is discussed in detail, as are effective diffusivities of buoyancy and momentum. Entrainment rates are compared with results from laboratory experiments. The results suggest that the ratio of the thicknesses of the shear layer and the stratified layer is a key parameter controlling mixing. With that ratio held constant, KH billows mix more rapidly than do Holmboe waves. Among Holmboe waves, mixing increases with increasing density difference, despite the fact that the transition to turbulence is delayed or prevented entirely by the stratification. Results are summarized in parameterizations of the effective viscosity and diffusivity of Holmboe waves.
publisherAmerican Meteorological Society
titleMixing in Symmetric Holmboe Waves
typeJournal Paper
journal volume37
journal issue6
journal titleJournal of Physical Oceanography
identifier doi10.1175/JPO3037.1
journal fristpage1566
journal lastpage1583
treeJournal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 006
contenttypeFulltext


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