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contributor authorSimeonov, Julian
contributor authorStern, Melvin
date accessioned2017-06-09T14:56:31Z
date available2017-06-09T14:56:31Z
date copyright2004/07/01
date issued2004
identifier issn0022-3670
identifier otherams-30092.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4167393
description abstractA density-compensated thermohaline front with a finite width L? and total lateral salinity variation ?S superimposed on a finger-favorable thermocline is studied by means of linear theory and nonlinear numerical calculations using parameterized finger fluxes. By retaining the relatively small molecular heat diffusion and the dependence of the finger Nusselt number Nu on the density ratio, it is shown that marginal stability with critical ?S is possible. The lateral fluxes induce a mean vertical velocity w0(x), which can sharpen the front, but when ?S exceeds a certain value the effect of the lateral fluxes exceeds that of w0(x) and the front weakens. Nonlinear 2D spectral calculations showed that the modification of the mean horizontal gradients is small and that the intrusions continue to grow exponentially even after they have produced overturns. By extrapolating the linear theory results beyond the overturning stage, the intrusion velocity was estimated to be proportional to the Brunt?Väisälä frequency multiplied by the intrusion thickness.
publisherAmerican Meteorological Society
titleDouble-Diffusive Intrusions on a Finite-Width Thermohaline Front
typeJournal Paper
journal volume34
journal issue7
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(2004)034<1723:DIOAFT>2.0.CO;2
journal fristpage1723
journal lastpage1740
treeJournal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 007
contenttypeFulltext


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