Abstract
We start here with the equation (14,21) for the function δ(x, z), which is the displacement of a particle above its equilibrium height (in the steady case).
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(1991). Miscellanea. In: Meteorological Fluid Dynamics. Lecture Notes in Physics Monographs, vol 5. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-38386-4_10
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