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AMS Glossary
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Section DD index151-159 of 573 terms

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  • depletion curve—That portion of a hydrograph in which streamflow comes primarily from groundwater seepage, resulting in depletion of the groundwater (or lake water, swamp water) reservoir.
    See recession curve.
  • depolarization ratio—General term denoting the ratio of the cross-polarized to the copolarized signal components measured by a polarimetric radar.
    See circular depolarization ratio, linear depolarization ratio, elliptical depolarization ratio.
  • depolarization—The process by which a polarized signal, for example, a radar signal, loses its original polarization as the result of scattering or of propagation through an anisotropic medium.
    The signal may experience a change of polarization, for example, from circular to elliptical as a result of differential attenuation or differential phase shift, or it may experience a loss of polarization, that is, become unpolarized, as a result of scattering in a random medium.
  • deposit gauge—The general name for instruments used in air pollution studies for determining the amount of material deposited on a given area during a given time.
  • deposition nucleus—A solid aerosol particle that nucleates an ice crystal directly from the vapor, particularly (but not necessarily) at subwater saturation and in the absence of the bulk liquid phase.
    The process does not preclude an intermediate adsorbed layer (Langmuir layer) prior to nucleation.
  • deposition velocity—In dry deposition, the quotient of the flux of a particular species to the surface (in units of concentration per unit area per unit time) and the concentration of the species at a specified reference height, typically 1 m.
    Typical deposition velocities for common gas phase pollutants (e.g., ozone, nitric acid) are of order 0.01–5 cm s−1.
  • deposition—Processes by which traces gases or particles are transferred from the atmosphere to the surface of the earth.
    Atmospheric deposition is usually divided into two categories, wet deposition and dry deposition, depending on the phase of the material during the deposition process. Thus, in wet deposition, the gas or particle is first incorporated into a droplet and is then transferred to the surface via precipitation. In dry deposition, the gas or particle is transported to ground level, where it is adsorbed onto a surface. The surface can be the ocean, soil, vegetation, buildings, etc. Note that the surface involved in the dry deposition may be wet or dry—the “dry” in dry deposition refers only to the phase of the material being deposited.
  • depression angle—(Also called depression.) The angle between the horizon and a point below, measured along the arc that passes through the point in question and is perpendicular to the horizon.
    The depression angle is the zenith distance of the point in question minus 90°. Compare azimuth, elevation angle, zenith distance.
  • depression of the dewpoint—See dewpoint depression.
  • depression storage—Water temporarily retained in puddles, ditches, and other depressions in the surface of the ground, and eventually evaporated or infiltrated; the small-scale counterpart of closed drainage.

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