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    Advances in Predicting Continental Low Stratus with a Regional NWP Model

    Source: Weather and Forecasting:;2010:;volume( 025 ):;issue: 001::page 290
    Author:
    Kann, Alexander
    ,
    Seidl, Harald
    ,
    Wittmann, Christoph
    ,
    Haiden, Thomas
    DOI: 10.1175/2009WAF2222314.1
    Publisher: American Meteorological Society
    Abstract: In the eastern Alpine region, subinversion cloudiness associated with elevated temperature inversions is a frequent phenomenon in autumn and winter, which often persists for several days. Although the prediction of fog and low stratus by numerical weather prediction (NWP) models has improved in recent years, these models still show deficiencies in the spatial and temporal evolution of such wintertime weather phenomena. In spite of sophisticated current assimilation schemes or simply due to unknown conditions, even the analysis shows large discrepancies compared to the true atmospheric state. Inversions are often ?smeared out? and the moist layer below the inversion is too far from saturation. Model integration from such an initial state leads to strong biases in the total cloudiness and, due to erroneous radiative response, in 2-m temperature forecasts. In the present paper, an empirical enhancement scheme for subinversion cloudiness is introduced within the framework of Aire Limitée Adaptation Dynamique Développement International (ALADIN), the operational limited area model (LAM) at the Austrian Central Institute for Meteorology and Geodynamics (ZAMG). The scheme attempts to compensate for model deficiencies in the vertical temperature and humidity profiles in order to enhance or keep preexisting signals of inversions and associated low cloudiness. Thus, a positive feedback due to radiative reaction is activated, which finally leads to more realistic vertical profiles, low (and total) cloudiness, and improved 2-m temperature predictions. Case studies demonstrate the impacts of the scheme on predictions of the spatial distribution of low cloudiness and on the vertical profiles of temperature and humidity. Verification over stratus episodes within a 2-month period comparing a reference model run without the scheme with a modified model version with the subinversion cloudiness scheme confirms the ability of the scheme to improve stratus-related wintertime weather prediction.
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      Advances in Predicting Continental Low Stratus with a Regional NWP Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4211493
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    • Weather and Forecasting

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    contributor authorKann, Alexander
    contributor authorSeidl, Harald
    contributor authorWittmann, Christoph
    contributor authorHaiden, Thomas
    date accessioned2017-06-09T16:32:56Z
    date available2017-06-09T16:32:56Z
    date copyright2010/02/01
    date issued2010
    identifier issn0882-8156
    identifier otherams-69786.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211493
    description abstractIn the eastern Alpine region, subinversion cloudiness associated with elevated temperature inversions is a frequent phenomenon in autumn and winter, which often persists for several days. Although the prediction of fog and low stratus by numerical weather prediction (NWP) models has improved in recent years, these models still show deficiencies in the spatial and temporal evolution of such wintertime weather phenomena. In spite of sophisticated current assimilation schemes or simply due to unknown conditions, even the analysis shows large discrepancies compared to the true atmospheric state. Inversions are often ?smeared out? and the moist layer below the inversion is too far from saturation. Model integration from such an initial state leads to strong biases in the total cloudiness and, due to erroneous radiative response, in 2-m temperature forecasts. In the present paper, an empirical enhancement scheme for subinversion cloudiness is introduced within the framework of Aire Limitée Adaptation Dynamique Développement International (ALADIN), the operational limited area model (LAM) at the Austrian Central Institute for Meteorology and Geodynamics (ZAMG). The scheme attempts to compensate for model deficiencies in the vertical temperature and humidity profiles in order to enhance or keep preexisting signals of inversions and associated low cloudiness. Thus, a positive feedback due to radiative reaction is activated, which finally leads to more realistic vertical profiles, low (and total) cloudiness, and improved 2-m temperature predictions. Case studies demonstrate the impacts of the scheme on predictions of the spatial distribution of low cloudiness and on the vertical profiles of temperature and humidity. Verification over stratus episodes within a 2-month period comparing a reference model run without the scheme with a modified model version with the subinversion cloudiness scheme confirms the ability of the scheme to improve stratus-related wintertime weather prediction.
    publisherAmerican Meteorological Society
    titleAdvances in Predicting Continental Low Stratus with a Regional NWP Model
    typeJournal Paper
    journal volume25
    journal issue1
    journal titleWeather and Forecasting
    identifier doi10.1175/2009WAF2222314.1
    journal fristpage290
    journal lastpage302
    treeWeather and Forecasting:;2010:;volume( 025 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian