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    Peak Reading and Thresholding in Processing Radar Weather Data 

    Source: Journal of Applied Meteorology:;1971:;volume( 010 ):;issue: 006:;page 1213
    Author(s): Marshall, J. S.
    Publisher: American Meteorological Society
    Abstract: A new PPI map is made up of 600 radial lines, each of 100 dots. Each dot is in one of six shades of grey, thus indicating target intensity, and dot size varies somewhat with shade. Each dot combines k independent data, ...
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    PRECIPITATION TRAJECTORIES AND PATTERNS 

    Source: Journal of Meteorology:;1953:;volume( 010 ):;issue: 001:;page 25
    Author(s): Marshall, J. S.
    Publisher: American Meteorological Society
    Abstract: A characteristic ?mares' tail? pattern of falling snow (observed in vertical section by radar) suggests that the snow is generated continuously, in compact generating elements; the pattern results from the snow's falling ...
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    Power-Law Relations in Radar Meteorology 

    Source: Journal of Applied Meteorology:;1969:;volume( 008 ):;issue: 001:;page 171
    Author(s): Marshall, J. S.
    Publisher: American Meteorological Society
    Abstract: tract
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    Radar Precipitation Maps as Lightning Indicators 

    Source: Journal of Applied Meteorology:;1978:;volume( 017 ):;issue: 002:;page 206
    Author(s): Marshall, J. S.; Radhakant, S.
    Publisher: American Meteorological Society
    Abstract: Radar maps of precipitation at a height of 6 km have been studied for the thunderstorms of one July day. Regions on these maps within which the intensity level exceeds 30 dBZ (corresponding to a rainfall rate of 2.8 mm ...
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    Structure and Dynamics of Bounded Vortex Flows With Different Nozzle Heights 

    Source: Journal of Fluids Engineering:;2015:;volume( 137 ):;issue: 010:;page 101202
    Author(s): Green, A. M.; Marshall, J. S.
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: A bounded vortex flow is generated by a nozzle with a central suction outlet surrounded by inlet jets with a 15 deg inclination in the azimuthal direction. The jets impinge on a flat surface called the impingement surface. ...
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    PATTERN ANALYSIS OF ONE SUMMER'S MULTILEVEL MAPS OF MONTREAL RAIN 

    Source: Monthly Weather Review:;1970:;volume( 098 ):;issue: 005:;page 335
    Author(s): MARSHALL, J. S.; HOLTZ, C. D.
    Publisher: American Meteorological Society
    Abstract: For the summer of 1964, precipitation intensity in the vicinity of Montreal, observed by CPS-9 radar, was recorded on constant-altitude maps at six heights. To allow for attenuation (at ??=?3.2 cm) and other radar ...
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    Measurement of Snowfall by Radar 

    Source: Journal of Applied Meteorology:;1972:;volume( 011 ):;issue: 003:;page 494
    Author(s): Carlson, Paul E.; Marshall, J. S.
    Publisher: American Meteorological Society
    Abstract: Using a CPS-9 radar (wavelength 3.2 cm, beamwidth 1°) in dry snow, radar returns from a layer at an average height of 5000 ft were converted to snowfall rates (taking Z?R2.0) and summed over 36 hr to obtain a map of snowfall ...
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    A THEORY OF SNOW-CRYSTAL HABIT AND GROWTH 

    Source: Journal of Meteorology:;1954:;volume( 011 ):;issue: 002:;page 104
    Author(s): Marshall, J. S.; Langleben, M. P.
    Publisher: American Meteorological Society
    Abstract: Strong evidence, available from the experiments of Nakaya and his co-workers and bolstered by an analogue experiment, supports the argument that type of snow-crystal growth is determined principally by the excess of the ...
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    MEASUREMENT OF SNOW PARAMETERS BY RADAR 

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 005:;page 322
    Author(s): Marshall, J. S.; Gunn, K. L. S.
    Publisher: American Meteorological Society
    Abstract: According to Rayleigh scattering theory for small spheres, back scattering is proportional to |K2Z where K is the dielectric factor and Z is the sum of the sixth powers of the diameter D. For small non-spherical particles ...
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    THE EFFECT OF WIND SHEAR ON FALLING PRECIPITATION 

    Source: Journal of Meteorology:;1955:;volume( 012 ):;issue: 004:;page 339
    Author(s): Gunn, K. L. S.; Marshall, J. S.
    Publisher: American Meteorological Society
    Abstract: Precipitation particles which fall from a source aloft through a wind shear are sorted as to size, the largest particles reaching the ground closest to the generating source, the smaller particles further from it. If ...
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