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    Vertical Motions Estimated Using Data from a Single Station and a Form of the Adiabatic Method 

    Source: Journal of Applied Meteorology:;1994:;volume( 033 ):;issue: 001:;page 65
    Author(s): Nastrom, G. D.; Warnock, J. M.
    Publisher: American Meteorological Society
    Abstract: The so-called adiabatic method for estimating vertical air motions under isentropic flow conditions can be used with wind and temperature data from a single station. With the advent of radio acoustic sounding systems, wind ...
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    Measurement of Synoptic-Scale Vertical Velocities by Two Nearby VHF Doppler Radars in Very Flat Terrain 

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 001:;page 5
    Author(s): Warnock, J. M.; VanZandt, T. E.; Clark, W. L.; Franke, S. J.; Kim, H. S.; Nastrom, G. D.; Johnston, P. E.
    Publisher: American Meteorological Society
    Abstract: An experimental field campaign to measure synoptic-scale vertical velocities was conducted from 5 to 11 January 1991 in the Urbana-Champaign, Illinois, region, which is in very flat terrain far from mountains. Both the ...
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    Case Studies of the Vertical Velocity Seen by the Flatland Radar Compared with Indirectly Computed Values 

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 001:;page 14
    Author(s): Nastrom, G. D.; Clark, W. L.; Gage, K. S.; VanZandt, T. E.; Warnock, J. M.; Creasey, R.; Pauley, P. M.
    Publisher: American Meteorological Society
    Abstract: The hypothesis that temporal averages of vertical motions over a single radar station are representative of weather systems large enough to be resolved by the radiosonde network is tested using data from the Flatland VHF ...
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