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    An Analytical Study of Nonlinear Responses of Rising Balloons to Horizontal Winds 

    Source: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 003:;page 413
    Author(s): Nastrom, G. D.; VanZandt, T. E.
    Publisher: American Meteorological Society
    Abstract: Solutions of the nonlinear, coupled equations of horizontal and vertical balloon motions are obtained using standard expansion methods. Comparison of the results of these solutions with those from numerical integration and ...
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    Mean Vertical Motions Seen by Radar Wind Profilers 

    Source: Journal of Applied Meteorology:;1994:;volume( 033 ):;issue: 008:;page 984
    Author(s): Nastrom, G. D.; VanZandt, T. E.
    Publisher: American Meteorological Society
    Abstract: Radar wind profilers have been used to measure directly the vertical motion above the radar site. Mean values of vertical motions in the troposphere and lower stratosphere reported at sites in and near mountains are often ...
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    Biases Due to Gravity Waves in Wind Profiler Measurements of Winds 

    Source: Journal of Applied Meteorology:;1996:;volume( 035 ):;issue: 002:;page 243
    Author(s): Nastrom, G. D.; VanZandt, T. E.
    Publisher: American Meteorological Society
    Abstract: Radar reflectivity for Bragg scattering is proportional to the atmospheric static stability. In vertically propagating gravity waves the perturbations to the static stability and to the winds occur either in phase or out ...
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    VHF Doppler Radar Observations of Buoyancy Waves Associated with Thunderstorms 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 002:;page 272
    Author(s): Lu, Daren; VanZandt, T. E.; Clark, W. L.
    Publisher: American Meteorological Society
    Abstract: The Platteville VHF Doppler radar, located on the Colorado piedmont near Platteville, Colorado, continuously measured the vertical wind velocity during a 12-day period in late July and early August 1981. Measurements were ...
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    MST Radar Observations of a Saturated Gravity Wave Spectrum 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 015:;page 2440
    Author(s): Tsuda, T.; Inoue, T.; Kato, S.; Fukao, S.; Fritts, D. C.; VanZandt, T. E.
    Publisher: American Meteorological Society
    Abstract: We present vertical wavenumber spectra of mesoscale wind fluctuations using data observed in the troposphere, lower stratosphere and mesosphere by the MU radar at 35°N in Japan in October 1986 and June 1987, as well as ...
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    Gravity Waves and Convection in Colorado during July 1983 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 011:;page 1534
    Author(s): Einaudi, F.; Clark, W. L.; Green, J. L.; VanZandt, T. E.; Fua, D.
    Publisher: American Meteorological Society
    Abstract: In order to gain insight into the complex dynamics of a convective system interacting with a gravity wave train, we have carried out an experiment in northeast Colorado during July and August, 1983, utilizing data from ...
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    Sources of Gravity Wave Activity Seen in the Vertical Velocities Observed by the Flatland VHF Radar 

    Source: Journal of Applied Meteorology:;1990:;volume( 029 ):;issue: 008:;page 783
    Author(s): Nastrom, G. D.; Peterson, M. R.; Green, J. L.; Gage, K. S.; VanZandt, T. E.
    Publisher: American Meteorological Society
    Abstract: Observations of vertical velocity made with the Flatland VHF radar located in the extremely flat terrain near Champaign, Illinois, are used to study sources of enhanced variance. The variance is used as an indicator of ...
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    Studies of Velocity Fluctuations in the Lower Atmosphere Using the MU Radar. Part I: Azimuthal Anisotropy 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 001:;page 39
    Author(s): VanZandt, T. E.; Smith, S. A.; Tsuda, T.; Sato, T.; Fukao, S.; Kato, S.; Fritts, D. C.
    Publisher: American Meteorological Society
    Abstract: We present in this paper a study of the azimuthal anisotropy of the motion field observed during a six-day campaign in March 1986 using the MU radar in Shigaraki, Japan. The radial wind velocity was observed at 20° zenith ...
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    A 4-yr Climatology of Pressure Disturbances Using a Barometer Network in Central Illinois 

    Source: Monthly Weather Review:;1999:;volume( 127 ):;issue: 007:;page 1613
    Author(s): Grivet-Talocia, S.; Einaudi, F.; Clark, W. L.; Dennett, R. D.; Nastrom, G. D.; VanZandt, T. E.
    Publisher: American Meteorological Society
    Abstract: This paper presents a climatology of coherent disturbances detected during 1991?95 by a network of barometers with a diameter of about 50 km located in a very flat terrain centered on the Flatland Atmospheric Observatory ...
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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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