The analogy between streamline curvature and buoyancy in turbulent shear flow

書誌事項

公開日
1969-03-27
権利情報
  • https://www.cambridge.org/core/terms
DOI
  • 10.1017/s0022112069001583
公開者
Cambridge University Press (CUP)

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説明

<jats:p>A formal algebraic analogy is drawn between meteorological parameters, such as the Richardson number, and the parameters describing the effect of rotation or streamline curvature on a turbulent flow. The analogy between the<jats:italic>phenomena</jats:italic>is a good first approximation. Semi-quantitative use of the analogy to apply meteorological data to curved shear layers shows that the effects of curvature on the apparent mixing length are appreciable if the shear-layer thickness exceeds roughly 1/300 of the radius of curvature; larger effects may occur in compressible flow. Application of the Monin-Oboukhov formula considerably improves the agreement between prediction and experiment in boundary layers on curved surfaces.</jats:p>

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