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    A Meteorological Distribution System for High-Resolution Terrestrial Modeling (MicroMet)

    Source: Journal of Hydrometeorology:;2006:;Volume( 007 ):;issue: 002::page 217
    Author:
    Liston, Glen E.
    ,
    Elder, Kelly
    DOI: 10.1175/JHM486.1
    Publisher: American Meteorological Society
    Abstract: An intermediate-complexity, quasi?physically based, meteorological model (MicroMet) has been developed to produce high-resolution (e.g., 30-m to 1-km horizontal grid increment) atmospheric forcings required to run spatially distributed terrestrial models over a wide variety of landscapes. The following eight variables, required to run most terrestrial models, are distributed: air temperature, relative humidity, wind speed, wind direction, incoming solar radiation, incoming longwave radiation, surface pressure, and precipitation. To produce these distributions, MicroMet assumes that at least one value of each of the following meteorological variables are available for each time step, somewhere within, or near, the simulation domain: air temperature, relative humidity, wind speed, wind direction, and precipitation. These variables are collected at most meteorological stations. For the incoming solar and longwave radiation, and surface pressure, either MicroMet can use its submodels to generate these fields, or it can create the distributions from observations as part of a data assimilation procedure. MicroMet includes a preprocessor component that analyzes meteorological data, then identifies and corrects potential deficiencies. Since providing temporally and spatially continuous atmospheric forcing data for terrestrial models is a core objective of MicroMet, the preprocessor also fills in any missing data segments with realistic values. Data filling is achieved by employing a variety of procedures, including an autoregressive integrated moving average calculation for diurnally varying variables (e.g., air temperature). To create the distributed atmospheric fields, spatial interpolations are performed using the Barnes objective analysis scheme, and subsequent corrections are made to the interpolated fields using known temperature?elevation, wind?topography, humidity?cloudiness, and radiation?cloud?topography relationships.
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      A Meteorological Distribution System for High-Resolution Terrestrial Modeling (MicroMet)

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4224501
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    contributor authorListon, Glen E.
    contributor authorElder, Kelly
    date accessioned2017-06-09T17:13:54Z
    date available2017-06-09T17:13:54Z
    date copyright2006/04/01
    date issued2006
    identifier issn1525-755X
    identifier otherams-81492.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4224501
    description abstractAn intermediate-complexity, quasi?physically based, meteorological model (MicroMet) has been developed to produce high-resolution (e.g., 30-m to 1-km horizontal grid increment) atmospheric forcings required to run spatially distributed terrestrial models over a wide variety of landscapes. The following eight variables, required to run most terrestrial models, are distributed: air temperature, relative humidity, wind speed, wind direction, incoming solar radiation, incoming longwave radiation, surface pressure, and precipitation. To produce these distributions, MicroMet assumes that at least one value of each of the following meteorological variables are available for each time step, somewhere within, or near, the simulation domain: air temperature, relative humidity, wind speed, wind direction, and precipitation. These variables are collected at most meteorological stations. For the incoming solar and longwave radiation, and surface pressure, either MicroMet can use its submodels to generate these fields, or it can create the distributions from observations as part of a data assimilation procedure. MicroMet includes a preprocessor component that analyzes meteorological data, then identifies and corrects potential deficiencies. Since providing temporally and spatially continuous atmospheric forcing data for terrestrial models is a core objective of MicroMet, the preprocessor also fills in any missing data segments with realistic values. Data filling is achieved by employing a variety of procedures, including an autoregressive integrated moving average calculation for diurnally varying variables (e.g., air temperature). To create the distributed atmospheric fields, spatial interpolations are performed using the Barnes objective analysis scheme, and subsequent corrections are made to the interpolated fields using known temperature?elevation, wind?topography, humidity?cloudiness, and radiation?cloud?topography relationships.
    publisherAmerican Meteorological Society
    titleA Meteorological Distribution System for High-Resolution Terrestrial Modeling (MicroMet)
    typeJournal Paper
    journal volume7
    journal issue2
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM486.1
    journal fristpage217
    journal lastpage234
    treeJournal of Hydrometeorology:;2006:;Volume( 007 ):;issue: 002
    contenttypeFulltext
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    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian