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    Meteorological Value of Ground Target Measurements by Radar 

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 004:;page 560
    Author(s): Fabry, Frédéric
    Publisher: American Meteorological Society
    Abstract: Many characteristics of radar echoes from ground targets vary with time as the properties of the atmosphere in which the radar waves propagate evolve. For example, if the phase of a target varies with time and the target ...
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    For How Long Should What Data Be Assimilated for the Mesoscale Forecasting of Convection and Why? Part II: On the Observation Signal from Different Sensors 

    Source: Monthly Weather Review:;2010:;volume( 138 ):;issue: 001:;page 256
    Author(s): Fabry, Frédéric
    Publisher: American Meteorological Society
    Abstract: The ability of data assimilation to correct for initial conditions depends on the presence of a usable signal in the variables observed as well as on the capability of instruments to detect that signal. In Part I, the ...
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    The Spatial Variability of Moisture in the Boundary Layer and Its Effect on Convection Initiation: Project-Long Characterization 

    Source: Monthly Weather Review:;2006:;volume( 134 ):;issue: 001:;page 79
    Author(s): Fabry, Frédéric
    Publisher: American Meteorological Society
    Abstract: An attempt was made to statistically gauge the importance of moisture variability on convection initiation by analyzing data collected by radar, surface stations, soundings, and airborne in situ sensors over the 7 weeks ...
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    Long-Term Radar Observations of the Melting Layer of Precipitation and Their Interpretation 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 007:;page 838
    Author(s): Fabry, Frederic; Zawadzki, Isztar
    Publisher: American Meteorological Society
    Abstract: In this study, 600 h of vertically pointing X-band radar data and 50 h of UHF boundary layer wind profiler data were processed and analyzed to characterize quantitatively the structure and the causes of the radar signature ...
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    Modeling of the Melting Layer. Part II: Electromagnetic 

    Source: Journal of the Atmospheric Sciences:;1999:;Volume( 056 ):;issue: 020:;page 3593
    Author(s): Fabry, Frédéric; Szyrmer, Wanda
    Publisher: American Meteorological Society
    Abstract: To complement the meteorological modeling of the melting layer, a model of the scattering properties at microwave frequencies for snow, melting snow, and rain is implemented. The scattering model, running in tandem with a ...
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    For How Long Should What Data Be Assimilated for the Mesoscale Forecasting of Convection and Why? Part I: On the Propagation of Initial Condition Errors and Their Implications for Data Assimilation 

    Source: Monthly Weather Review:;2010:;volume( 138 ):;issue: 001:;page 242
    Author(s): Fabry, Frédéric; Sun, Juanzhen
    Publisher: American Meteorological Society
    Abstract: Data assimilation is used among other things to constrain the initial conditions of weather forecasting models by fitting the model fields to observations made over a certain time interval. In particular, it tries to tie ...
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    Simulation and Interpretation of the Phase Data Used by the Radar Refractivity Retrieval Algorithm 

    Source: Journal of Atmospheric and Oceanic Technology:;2010:;volume( 027 ):;issue: 008:;page 1286
    Author(s): Park, Shinju; Fabry, Frédéric
    Publisher: American Meteorological Society
    Abstract: The radar refractivity retrieval algorithm applied to radar phase measurements from ground targets can provide high-resolution, near-surface moisture estimates in time and space. The reliability of the retrieval depends ...
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    Real-Time Radar Reflectivity Calibration from Differential Phase Measurements 

    Source: Journal of Atmospheric and Oceanic Technology:;2014:;volume( 031 ):;issue: 005:;page 1089
    Author(s): Bellon, Aldo; Fabry, Frédéric
    Publisher: American Meteorological Society
    Abstract: n algorithm based on the self-consistency between the horizontal reflectivity ZH and the specific differential phase KDP has been devised for the calibration of the reflectivity measurements of the McGill S-band dual-polarization ...
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    Why Scanning Instruments Are a Necessity for Constraining Temperature and Humidity Fields in the Lower Atmosphere 

    Source: Journal of Atmospheric and Oceanic Technology:;2014:;volume( 031 ):;issue: 011:;page 2462
    Author(s): Themens, David; Fabry, Frédéric
    Publisher: American Meteorological Society
    Abstract: he ability of different ground-based measurement strategies for constraining thermodynamic variables in the troposphere, particularly at the mesoscale, is investigated. First, a preliminary assessment of the capability of ...
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    Estimation of Near-Ground Propagation Conditions Using Radar Ground Echo Coverage 

    Source: Journal of Atmospheric and Oceanic Technology:;2010:;volume( 028 ):;issue: 002:;page 165
    Author(s): Park, Shinju; Fabry, Frédéric
    Publisher: American Meteorological Society
    Abstract: The vertical gradient of refractivity (dN/dh) determines the path of the radar beam; namely, the larger the negative values of the refractivity gradient, the more the beam bends toward the ground. The variability of the ...
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