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    Improved Retrieval of Integrated Water Vapor from Water Vapor Radiometer Measurements Using Numerical Weather Prediction Models

    Source: Journal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 005::page 1253
    Author:
    Chiswell, Steven R.
    ,
    Businger, Steven
    ,
    Bevis, Michael
    ,
    Solheim, Fredrick
    ,
    Rocken, Christian
    ,
    Ware, Randolph
    DOI: 10.1175/1520-0426(1994)011<1253:IROIWV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Water vapor radiometer (WVR) retrieval algorithms require a priori information on atmospheric conditions along the line of sight of the radiometer in order to derive opacities from observed brightness temperatures. This paper's focus is the mean radiating temperature of the atmosphere (Tmr), which is utilized in these algorithms to relate WVR measurements to integrated water vapor. Current methods for specifying Tmr rely on the climatology of the WVR site-for example, a seasonal average-or information from nearby soundings to specify Tmr. However, values of Tmr, calculated from radiosonde data, not only vary according to site and season but also exhibit large fluctuations in response to local weather conditions. By utilizing output from numerical weather prediction (NWP) models, Tmr can be accurately prescribed for an arbitrary WVR site at a specific time. Temporal variations in local weather conditions can he resolved by NWP models on timescales shorter than standard radiosonde soundings. Currently used methods for obtaining Tmr are reviewed. Values of Tmr obtained from current methods and this new approach are compared to those obtained from in situ radiosonde soundings. The improvement of the Tmr calculation using available model forecast data rather than climatological values yields a corresponding improvement of comparable magnitude in the retrieval of atmospheric opacity. Use of forecast model data relieves a WVR site of its dependency on local climatology or the necessity of a nearby sounding, allowing more accurate retrieval of observed conditions and increased flexibility in choosing site location. Furthermore, it is found that the calculation of precipitable water by means of atmospheric opacities does not require time-dependent tuning parameters when model data are used. These results were obtained using an archived subset of the full nested grid model output. The added horizontal and vertical resolution of operational data should further improve this approach.
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      Improved Retrieval of Integrated Water Vapor from Water Vapor Radiometer Measurements Using Numerical Weather Prediction Models

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4233217
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorChiswell, Steven R.
    contributor authorBusinger, Steven
    contributor authorBevis, Michael
    contributor authorSolheim, Fredrick
    contributor authorRocken, Christian
    contributor authorWare, Randolph
    date accessioned2017-06-09T17:40:02Z
    date available2017-06-09T17:40:02Z
    date copyright1994/10/01
    date issued1994
    identifier issn0739-0572
    identifier otherams-970.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233217
    description abstractWater vapor radiometer (WVR) retrieval algorithms require a priori information on atmospheric conditions along the line of sight of the radiometer in order to derive opacities from observed brightness temperatures. This paper's focus is the mean radiating temperature of the atmosphere (Tmr), which is utilized in these algorithms to relate WVR measurements to integrated water vapor. Current methods for specifying Tmr rely on the climatology of the WVR site-for example, a seasonal average-or information from nearby soundings to specify Tmr. However, values of Tmr, calculated from radiosonde data, not only vary according to site and season but also exhibit large fluctuations in response to local weather conditions. By utilizing output from numerical weather prediction (NWP) models, Tmr can be accurately prescribed for an arbitrary WVR site at a specific time. Temporal variations in local weather conditions can he resolved by NWP models on timescales shorter than standard radiosonde soundings. Currently used methods for obtaining Tmr are reviewed. Values of Tmr obtained from current methods and this new approach are compared to those obtained from in situ radiosonde soundings. The improvement of the Tmr calculation using available model forecast data rather than climatological values yields a corresponding improvement of comparable magnitude in the retrieval of atmospheric opacity. Use of forecast model data relieves a WVR site of its dependency on local climatology or the necessity of a nearby sounding, allowing more accurate retrieval of observed conditions and increased flexibility in choosing site location. Furthermore, it is found that the calculation of precipitable water by means of atmospheric opacities does not require time-dependent tuning parameters when model data are used. These results were obtained using an archived subset of the full nested grid model output. The added horizontal and vertical resolution of operational data should further improve this approach.
    publisherAmerican Meteorological Society
    titleImproved Retrieval of Integrated Water Vapor from Water Vapor Radiometer Measurements Using Numerical Weather Prediction Models
    typeJournal Paper
    journal volume11
    journal issue5
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1994)011<1253:IROIWV>2.0.CO;2
    journal fristpage1253
    journal lastpage1261
    treeJournal of Atmospheric and Oceanic Technology:;1994:;volume( 011 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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