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Section AA index171-179 of 917 terms

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  • adhesion efficiency—In cloud physics, the fraction of ice particles colliding with a collector ice particle that actually adheres to, or aggregates with, the collector; or, in the case of the riming process, the fraction of water drops colliding with a collector ice particle that actually adheres (freezes) to the collector.
  • adhesive water—Water retained by soil constituents as a result of the molecular attraction between the water and the soil.
  • adiabat—In most contexts, same as dry adiabat.
    See also saturation adiabat, pseudoadiabat.
  • adiabatic atmosphere—(Or dry-adiabatic atmosphere; also called convective atmosphere, homogeneous atmosphere.) A model atmosphere characterized by a dry-adiabatic lapse rate throughout its vertical extent.
    Such a condition is never observed and is also rather poorly designated, since “adiabatic” represents a process, not a condition. The pressure in an adiabatic atmosphere decreases with height according to

    where p0 and T0 are the pressure and temperature (K), respectively, at sea level, z the geometric height, Rd the gas constant for dry air, cpd the specific heat of dry air at constant pressure, and g the acceleration of gravity. See homogeneous atmosphere.
  • adiabatic chart—(Or adiabatic diagram.) Same as Stüve diagram, but often used synonymously with thermodynamic diagram.
  • adiabatic condensation pointSee lifting condensation level.
  • adiabatic condensation pressure—Same as condensation pressure.
  • adiabatic condensation temperature—Same as condensation temperature.
  • adiabatic coolingSee adiabatic process.
  • adiabatic diagram—Same as adiabatic chart.

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