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Finestructure, Microstructure, and Thin Layers     Microstructure  Thin Layers       font style='font-size:12px;'> 2015/8/6
We are all familiar with the irregular profiles from modern, high resolution conductivity-temperature-depth profilers (commonly called CTDs) freely falling vertical profilers, and towed thermistor cha...
Indonesian Seas Finestructure Variability     Indonesian Seas  Finestructure Variability       font style='font-size:12px;'> 2015/7/28
The Indonesian seas contain evidence of enhanced vertical mixing. Coupled with the highly stratified tropical thermocline, this enhanced mixing implies large vertical fluxes of heat and buoyancy from ...
Finestructure and microstructure observations of temperature and salinity were made over a two-week period in late winter at a site in the central North Pacific, during which time a mild storm, maximu...
Data obtained from the cycling mode of a towed system operated in the North Pacific are used to investigate the relationship of small-scale mixing to the finestructure which seems to be such a common ...
Large numbers of STD casts taken during five cruises to the same location in the central North Pacific permitted the separation of the temperature profile into mean T¯ (z) and fluctuating T′(z) c...
Discrimination between internal waves and finestructure in the ocean is made difficult because of over-lapping scales of each process. We have assumed as a working hypothesis that low frequency/wavenu...
Two hundred miles southwest of San Diego a conductivity/temperature/pressure instrument (CTD) was repeatedly raised and lowered to varying depths above 1000 m while under ship tow. Finestructure measu...
We have developed a statistical model describing a random field of internal waves passively oscillating a random, locally horizontally uniform temperature finestructure. Here we define finestructure t...
Reversible and Irreversible Finestructure     temperature profiles  Reversible  Irreversible Finestructure       font style='font-size:12px;'> 2009/2/9
Various statistics of temperature profiles are examined in an attempt to distinguish irreversible structures due to mixing from reversible distortions induced by internal wave straining. Even if all t...
We present and compare results from a two-dimensional numerical frontogenesis model and a field experiment in the eddy field of the North Atlantic Current in order to illustrate and explain the shape ...
Mesoscale turbulence is modeled in terms of an unstable potential vorticity front. The model integration starts from a purely zonal, 60-km-wide geostrophically balanced jet, on which is superimposed a...
Statistics of the Richardson Number:Mixing Models and Finestructure     Richardson Number  Mixing Models       font style='font-size:12px;'> 2008/12/10
Parameterization of the dissipation rate of turbulent kinetic energy () in terms of Richardson number (Ri = N2/S2) is examined for a variety in internal wave environments. Previous work with these dat...

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