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    The Accuracy of Vertical Air Velocities from Doppler Radar Data

    Source: Monthly Weather Review:;1998:;volume( 126 ):;issue: 001::page 92
    Author:
    Matejka, Thomas
    ,
    Bartels, Diana L.
    DOI: 10.1175/1520-0493(1998)126<0092:TAOVAV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Eight methods of calculating vertical air velocity in a column are compared. Each method requires some or all of the following data: horizontal divergence, vertical precipitation velocity, hydrometeor terminal fall speed, and vertical air velocity boundary conditions. Some or all of these quantities are commonly deduced or specified by a researcher during the analysis of Doppler radar data. The responses of the methods to different magnitudes and behaviors of errors in the input data are examined with a Monte Carlo method. The experiments are conducted with both random and systematic errors. Two idealized kinds of systematic errors are considered: bias error (a constant error through the column) and trend error (an error of constant magnitude that changes sign at the midpoint of the mass of the column). The performances of the methods are mapped over error space. A researcher, knowing approximately the characteristics of the errors of a particular set of Doppler radar data, can use the results of these experiments to select a method based on how well it performs in the presence of random errors and how well its performance holds up as bias and trend errors increase.
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      The Accuracy of Vertical Air Velocities from Doppler Radar Data

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4203997
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    contributor authorMatejka, Thomas
    contributor authorBartels, Diana L.
    date accessioned2017-06-09T16:11:43Z
    date available2017-06-09T16:11:43Z
    date copyright1998/01/01
    date issued1998
    identifier issn0027-0644
    identifier otherams-63038.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203997
    description abstractEight methods of calculating vertical air velocity in a column are compared. Each method requires some or all of the following data: horizontal divergence, vertical precipitation velocity, hydrometeor terminal fall speed, and vertical air velocity boundary conditions. Some or all of these quantities are commonly deduced or specified by a researcher during the analysis of Doppler radar data. The responses of the methods to different magnitudes and behaviors of errors in the input data are examined with a Monte Carlo method. The experiments are conducted with both random and systematic errors. Two idealized kinds of systematic errors are considered: bias error (a constant error through the column) and trend error (an error of constant magnitude that changes sign at the midpoint of the mass of the column). The performances of the methods are mapped over error space. A researcher, knowing approximately the characteristics of the errors of a particular set of Doppler radar data, can use the results of these experiments to select a method based on how well it performs in the presence of random errors and how well its performance holds up as bias and trend errors increase.
    publisherAmerican Meteorological Society
    titleThe Accuracy of Vertical Air Velocities from Doppler Radar Data
    typeJournal Paper
    journal volume126
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1998)126<0092:TAOVAV>2.0.CO;2
    journal fristpage92
    journal lastpage117
    treeMonthly Weather Review:;1998:;volume( 126 ):;issue: 001
    contenttypeFulltext
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