Abstract: The shape of the frontal or inversion surface over a lower moist layer with geostrophic wind balance is shown to be curved, and a steady-state distribution with a discontinuity in the shape of the surface is shown to be ...

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Abstract: No Abstract Available

Abstract: The almost complete mathematical analogy is established between incompressible flow of air under an inversion, and one- and two-dimensional flow of a compressible fluid at high speed. Some mathematical and graphical methods ...

Abstract: No Abstract Available