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    Validation of Cloud-Resolving Model Background Data for Cloud Data Assimilation

    Source: Monthly Weather Review:;2009:;volume( 138 ):;issue: 003::page 781
    Author:
    Polkinghorne, Rosanne
    ,
    Vukicevic, Tomislava
    ,
    Evans, K. Franklin
    DOI: 10.1175/2009MWR3012.1
    Publisher: American Meteorological Society
    Abstract: Results from a cloud-resolving model are systematically compared with a variety of observations, both ground based and satellite, in order to better understand the mean background errors and their correlations. This is a step in the direction of developing a background error covariance matrix for use in cloud data assimilation. Observation sources include the Geostationary Operational Environmental Satellite (GOES), the Atmospheric Emitted Radiance Interferometer (AERI), a microwave radiometer (MWR), radiosonde, and cloud radar. When exploring model biases in temperature, precipitable water vapor, and liquid water path, a warm and moist bias at night and a cool and dry bias during the day are observed. Values for the background decorrelation length of water variables are determined. In addition, a dynamic cloud mask is presented to give more control in the assimilation of cloudy satellite radiances, allowing different cloud types to be excluded from the assimilation as well as establishing values for the maximum residuals to be considered.
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      Validation of Cloud-Resolving Model Background Data for Cloud Data Assimilation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4211302
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    contributor authorPolkinghorne, Rosanne
    contributor authorVukicevic, Tomislava
    contributor authorEvans, K. Franklin
    date accessioned2017-06-09T16:32:18Z
    date available2017-06-09T16:32:18Z
    date copyright2010/03/01
    date issued2009
    identifier issn0027-0644
    identifier otherams-69613.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211302
    description abstractResults from a cloud-resolving model are systematically compared with a variety of observations, both ground based and satellite, in order to better understand the mean background errors and their correlations. This is a step in the direction of developing a background error covariance matrix for use in cloud data assimilation. Observation sources include the Geostationary Operational Environmental Satellite (GOES), the Atmospheric Emitted Radiance Interferometer (AERI), a microwave radiometer (MWR), radiosonde, and cloud radar. When exploring model biases in temperature, precipitable water vapor, and liquid water path, a warm and moist bias at night and a cool and dry bias during the day are observed. Values for the background decorrelation length of water variables are determined. In addition, a dynamic cloud mask is presented to give more control in the assimilation of cloudy satellite radiances, allowing different cloud types to be excluded from the assimilation as well as establishing values for the maximum residuals to be considered.
    publisherAmerican Meteorological Society
    titleValidation of Cloud-Resolving Model Background Data for Cloud Data Assimilation
    typeJournal Paper
    journal volume138
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/2009MWR3012.1
    journal fristpage781
    journal lastpage795
    treeMonthly Weather Review:;2009:;volume( 138 ):;issue: 003
    contenttypeFulltext
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