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Development of overturning circulation in sloping waterbodies due to surface cooling - MaRDI portal

Development of overturning circulation in sloping waterbodies due to surface cooling (Q5164696)

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scientific article; zbMATH DE number 7425745
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Development of overturning circulation in sloping waterbodies due to surface cooling
scientific article; zbMATH DE number 7425745

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    Development of overturning circulation in sloping waterbodies due to surface cooling (English)
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    12 November 2021
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    cavity convection
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    buoyancy-driven instability
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    topographic effect
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    thermal siphon model
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    air-water interface
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    stratified basin
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    cross-shore pressure gradient
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