Gilman and Benton have demonstrated the existence of composite Ekman‐Hartmann layer flow in rotating, electrically conducting fluids permeated by a magnetic field normal to the boundary. This flow was shown to evolve smoothly from a pure Ekman layer to a pure Hartmann layer as the parameter increases (μ is magnetic permeability, is density, is magnetic diffusivity, is the rotation rate, and is the imposed magnetic field). Here, it is shown that in the Cartesian, low magnetic Prandtl number limit, this flow exhibits the two instabilities to two‐dimensional rolls characteristic of the pure Ekman layer, but at Reynolds numbers that increase rapidly as increases. Both rolls decrease in horizontal scale, orient more nearly parallel to the flow far from the boundary, and acquire smaller phase velocities. Coriolis forces are seen to give a parallel roll instability of the Hartmann layer, at much lower Reynolds numbers than given by Roberts for Hartmann layer instability in the absence of rotation.
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January 1971
Research Article|
January 01 1971
Instabilities of the Ekman‐Hartmann Boundary Layer
Peter A. Gilman
Peter A. Gilman
Advanced Study Program National Center for Atmospheric Research, Boulder, Colorado 80302
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Peter A. Gilman
Advanced Study Program National Center for Atmospheric Research, Boulder, Colorado 80302
Phys. Fluids 14, 7–12 (1971)
Article history
Received:
May 21 1970
Citation
Peter A. Gilman; Instabilities of the Ekman‐Hartmann Boundary Layer. Phys. Fluids 1 January 1971; 14 (1): 7–12. https://doi.org/10.1063/1.1693290
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