Abstract
A description is given of the flow of a three-layer system of immiscible fluids over an obstacle immersed in the lowest liquid. A tentative suggestion is offered that some features of the motion may be similar to the flow of air over the Sierra range near Bishop, California. Some arguments are advanced supporting this suggestion.
Cite
CITATION STYLE
APA
Long, R. R. (1953). A Laboratory Model Resembling the “Bishop-Wave” Phenomenon. Bulletin of the American Meteorological Society, 34(5), 205–211. https://doi.org/10.1175/1520-0477-34.5.205
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