Estimates of the temperature flux–temperature gradient relation above a sea floor

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Estimates of the temperature flux–temperature gradient relation above a sea-floor

The relation between the flux of temperature (or buoyancy), the vertical temperature gradient and the height above the bottom, is investigated in an oceanographic context, using high-resolution temperature measurements. The model for the evolution of a stratified layer by Balmforth et al. (1998) is reviewed and adapted to the case of a turbulent flow above a wall. Model predictions are compared...

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ژورنال

عنوان ژورنال: Journal of Fluid Mechanics

سال: 2016

ISSN: 0022-1120,1469-7645

DOI: 10.1017/jfm.2016.112