Gradient Richardson Number is a dimensionless stability parameter in fluid dynamics that quantifies the ratio of buoyancy stabilization to shear destabilization in a stratified flow, defined as the ratio of the square of the buoyancy frequency to the square of the vertical shear of the horizontal velocity.
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Flux-Profile Relationships in the Atmospheric Surface Layer
J. A. Businger, J. C. Wyngaard, Yutaka Izumi et al. · Journal of the Atmospheric Sciences · 1971 · 3.3K citations · Full text
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University of Cambridge
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Tempe, United States
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Falmouth, United States
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NSF National Center for Atmospheric Research
Boulder, United States
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Cooperative Institute for Research in Environmental Sciences
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