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- W2040700424 abstract "The solution of a steady-state, baroclinic boundary layer over a two-dimensional terrain in an f plane is obtained. The boundary-layer thickness is found to be dependent on both the stability S = αmg[(Tm/H) + (g/cp)] (4Ω2L)−1 and the terrain slope. For a given terrain slope α and Prandtl number σ = ν/k, a critical value of the stability parameter S is found to exist and be equal to −(α2σ)−1, beyond which the O(1) boundary layer disappears completely. Except for neutral stability, the solution conserves up-slope (or down-slope) mass transport when the free-stream thermal wind is parallel to the ridges, reflecting the fact that the boundary layer is “leak free.” When the free stream possesses a small cross-ridge component, the Ekman suction is necessarily nonzero even under nonneutral conditions, so that the influx from the interior may be accommodated." @default.
- W2040700424 created "2016-06-24" @default.
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- W2040700424 date "1969-09-01" @default.
- W2040700424 modified "2023-09-23" @default.
- W2040700424 title "Buoyant Ekman Layer" @default.
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- W2040700424 doi "https://doi.org/10.1063/1.1692739" @default.
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