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First Edition Preface Second Edition Preface Acknowledgments
Section S S index 321-329 of 1376 terms
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shearing deformationSee deformation.
shearing instability1. Same as Helmholtz instability. 2. A complex hydrodynamic instability phenomenon exhibited by a stratified shear flow. A necessary condition for this type of instability is that the local Richardson number is somewhere less than one-quarter.
Drazin, P. G., and W. H. Reid, 1981: Hydrodynamic Stability, Cambridge University Press, 325–333.
shearing stressAny of the tangential components of the stress tensor. In meteorology, the shearing stress is often that on a horizontal surface in the direction of the wind: where μ is the dynamic (molecular) viscosity, u the wind speed, and z the vertical coordinate. A corresponding eddy stress, or Reynolds stress, may be defined, with an eddy viscosity in place of the molecular viscosity. See also surface friction, Newtonian friction law.
shearing waveSee transverse wave.
sheet erosion(Also called sheet wash.) Erosion of thin layers of earth-surface material, more or less evenly, from extended areas of gently sloping land by broad continuous sheets of running water, without the formation of rills, gullies, or other channelized flow.
sheet flowSame as laminar flow.
sheet frostA thick coating of rime formed on windows and other surfaces.
sheet iceIce formed in a smooth thin layer on a water surface by the coagulation of frazil through rapid freezing.
sheet lightning(Also called luminous cloud.) A diffuse, but sometimes fairly bright, illumination of those parts of a thundercloud that surround the path of a lightning flash, particularly a cloud discharge or cloud-to-cloud discharge. Thus, sheet lightning is no unique form of lightning but only one manifestation of ordinary lightning types in the presence of obscuring clouds. Compare heat lightning.
sheet washSame as sheet erosion.
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