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Section SS index321-329 of 1376 terms

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  • shearing deformationSee deformation.
  • shearing instability—1. 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 stress—Any 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 flow—Same as laminar flow.
  • sheet frost—A 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 wash—Same as sheet erosion.

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