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• W2023202033 abstract "We present new experimental results on the mechanisms through which steady two-dimensional density currents lead to the formation of a stratification in a closed basin. A motivation for this work is to test the underlying assumptions in a diffusive “filling box” model that describes the oceanic thermohaline circulation (Hughes, G.O. and Griffiths, R.W., A simple convective model of the global overturning circulation, including effects of entrainment into sinking regions, Ocean Modeling, 2005, submitted.). In particular, they hypothesized that a non-uniform upwelling velocity is due to weak along-slope entrainment in density currents associated with a large horizontal entrainment ratio of E eq  ∼ 0.1. We experimentally measure the relationship between the along-slope entrainment ratio, E, of a density current to the horizontal entrainment ratio, E eq, of an equivalent vertical plume. The along-slope entrainment ratios show the same quantitative decrease with slope as observed by Ellison and Turner (Ellison..." @default.
• W2023202033 created "2016-06-24" @default.
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• W2023202033 date "2005-06-01" @default.
• W2023202033 modified "2023-10-18" @default.
• W2023202033 title "Two-dimensional density currents in a confined basin" @default.
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• W2023202033 doi "https://doi.org/10.1080/03091920500094456" @default.
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