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Thermally enhanced gravity driven flows. (English) Zbl 1288.76014

Summary: Gravity currents play a major role in both natural and human-made settings. The driving buoyancy forces for these flows are due to density differences which may arise as a result of compositional differences (e.g. salinity), the presence of suspended material in the flow as in the case of turbidity currents, temperature differences, or a combination of these mechanisms. This article reports on a study of surface gravity currents moving horizontally over a slightly denser ambient fluid when these surface layers are subjected to an incoming heat flux which acts to enhance (or erode) the existing stratification. A general equation of state is adopted to connect the density of the upper layer to its changing temperature. A two-layer hydraulic theory is developed and conditions for its validity carefully specified. Both analytical and numerical analyses are carried out in order to examine the salient features of these flows.

MSC:

76B15 Water waves, gravity waves; dispersion and scattering, nonlinear interaction
35L65 Hyperbolic conservation laws
Full Text: DOI

References:

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