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    The Application of Radar Gauge Comparisons to Operational Precipitation Profile Corrections 

    Source: Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 012:;page 2612
    Author(s): Joss, Jürg; Lee, Robert
    Publisher: American Meteorological Society
    Abstract: The analyses of data recorded during the past eight years with two Swiss radars, a network of rain gauges, and river flow measurements have helped to quantify the vertical profile of reflectivity and the influences of ...
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    Mesobeta Profiles to Extrapolate Radar Precipitation Measurements above the Alps to the Ground Level 

    Source: Journal of Applied Meteorology:;2002:;volume( 041 ):;issue: 005:;page 542
    Author(s): Germann, Urs; Joss, Jürg
    Publisher: American Meteorological Society
    Abstract: In the Alps, the volume visible by a radar is reduced because of ground clutter, elevated horizon, and earth curvature. This often inhibits a direct view on precipitation close to the ground. When using radar measurements ...
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    Variograms of Radar Reflectivity to Describe the Spatial Continuity of Alpine Precipitation 

    Source: Journal of Applied Meteorology:;2001:;volume( 040 ):;issue: 006:;page 1042
    Author(s): Germann, Urs; Joss, Jürg
    Publisher: American Meteorological Society
    Abstract: The authors use variograms of radar reflectivity as a summary statistic to describe the spatial continuity of Alpine precipitation on mesogamma scales. First, how to obtain such variograms is discussed. Second, a set of ...
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    Experimental Determination of the Radar Cross Sections of Artificial Hailstones Containing Water 

    Source: Journal of Applied Meteorology:;1965:;volume( 004 ):;issue: 006:;page 723
    Author(s): Joss, Jürg; Aufdermaur, Armin N.
    Publisher: American Meteorological Society
    Abstract: The radar cross sections of particles grown in a hail tunnel (ice spheres with a spongy ice shell) and snow spheres dipped in water (spongy ice throughout) were measured at wavelengths of 3.21 cm, 4.67 cm, and 10 cm. The ...
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    Shapes of Raindrop Size Distributions 

    Source: Journal of Applied Meteorology:;1978:;volume( 017 ):;issue: 007:;page 1054
    Author(s): Joss, Jürg; Gori, Enrico G.
    Publisher: American Meteorological Society
    Abstract: The ?instant? shape of raindrop size distributions (measured during 1 min or less) usually differs from the exponential, generally in the direction of monodispersity. Experimental results are presented for both widespread ...
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    An Optical Disdrometer for Measuring Size and Velocity of Hydrometeors 

    Source: Journal of Atmospheric and Oceanic Technology:;2000:;volume( 017 ):;issue: 002:;page 130
    Author(s): Löffler-Mang, Martin; Joss, Jürg
    Publisher: American Meteorological Society
    Abstract: The characteristics of a prototype optical disdrometer are presented. Particles are detectable in the diameter range from 0.3 to 30 mm having velocities of up to 20 m s?1. Advantages of the new system are (i) it is easy ...
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    A Study of Sampling-Variability Effects in Raindrop Size Observations 

    Source: Journal of Applied Meteorology:;1993:;volume( 032 ):;issue: 007:;page 1259
    Author(s): Smith, Paul L.; Liu, Zhong; Joss, Jurg
    Publisher: American Meteorological Society
    Abstract: Because of the randomness associated with sampling from a population of raindrops, variations in the data reflect some undetermined mixture of sampling variability and inhomogeneity in the precipitation. Better understanding ...
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    A Water Hypsometer Utilizing High-Precision Thermocouples 

    Source: Journal of Atmospheric and Oceanic Technology:;1996:;volume( 013 ):;issue: 001:;page 175
    Author(s): Richner, Hans; Joss, Jürg; Ruppert, Paul
    Publisher: American Meteorological Society
    Abstract: A boiling-point barometer?commonly called hypsometer?has been developed for use on meteorological radiosondes. In this hypsometer, water is heated electrically, and its boiling temperature is measured with a thermocouple. ...
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    Three Methods to Determine Profiles of Reflectivity from Volumetric Radar Data to Correct Precipitation Estimates 

    Source: Journal of Applied Meteorology:;2000:;volume( 039 ):;issue: 010:;page 1715
    Author(s): Vignal, Bertrand; Galli, Gianmario; Joss, Jürg; Germann, Urs
    Publisher: American Meteorological Society
    Abstract: The vertical variability of radar reflectivity reduces the reliability of precipitation estimation by radar, especially in complex orography. This important source of error can, at least partially, be corrected for, if the ...
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    DSpace software copyright © 2002-2015  DuraSpace
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