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    WRF–SBM Simulations of Melting-Layer Structure in Mixed-Phase Precipitation Events Observed during LPVEx

    Source: Journal of Applied Meteorology and Climatology:;2014:;volume( 053 ):;issue: 012::page 2710
    Author:
    Iguchi, Takamichi
    ,
    Matsui, Toshihisa
    ,
    Tao, Wei-Kuo
    ,
    Khain, Alexander P.
    ,
    Phillips, Vaughan T. J.
    ,
    Kidd, Chris
    ,
    L’Ecuyer, Tristan
    ,
    Braun, Scott A.
    ,
    Hou, Arthur
    DOI: 10.1175/JAMC-D-13-0334.1
    Publisher: American Meteorological Society
    Abstract: wo mixed-phase precipitation events were observed on 21 September and 20 October 2010 over the southern part of Finland during the Light Precipitation Validation Experiment (LPVEx). These events have been simulated using the Weather Research and Forecasting Model coupled with spectral bin microphysics (WRF?SBM). The detailed ice-melting scheme with prognosis of the liquid water fraction during melting enables explicit simulation of microphysical properties in the melting layer. First, the simulations have been compared with C-band 3D radar measurements for the purpose of evaluating the overall profiles of cloud and precipitation. The simulation has some artificial convective patterns and errors in the forecast displacement of the precipitation system. The overall overestimation of reflectivity is consistent with a bias toward the range characterized by large-diameter droplets in the surface drop size distribution. Second, the structure of the melting bands has been evaluated against vertically pointing K-band radar measurements. A peak in reflectivity and a gradual change in Doppler velocity are observed and similarly simulated in the common temperature range from approximately 0° to 3°C. The effectiveness of the time-dependent melting scheme has been justified by intercomparison with a corresponding simulation using an instantaneous melting scheme. A weakness of the new melting scheme is that melting particles having high liquid water fractions on the order of 80%?90% cannot be simulated. This situation may cause underestimation of radar reflectivity in the melting layer because of the assumptions of melting-particle structure used to calculate the scattering properties.
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      WRF–SBM Simulations of Melting-Layer Structure in Mixed-Phase Precipitation Events Observed during LPVEx

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4217243
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    • Journal of Applied Meteorology and Climatology

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    contributor authorIguchi, Takamichi
    contributor authorMatsui, Toshihisa
    contributor authorTao, Wei-Kuo
    contributor authorKhain, Alexander P.
    contributor authorPhillips, Vaughan T. J.
    contributor authorKidd, Chris
    contributor authorL’Ecuyer, Tristan
    contributor authorBraun, Scott A.
    contributor authorHou, Arthur
    date accessioned2017-06-09T16:50:01Z
    date available2017-06-09T16:50:01Z
    date copyright2014/12/01
    date issued2014
    identifier issn1558-8424
    identifier otherams-74961.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217243
    description abstractwo mixed-phase precipitation events were observed on 21 September and 20 October 2010 over the southern part of Finland during the Light Precipitation Validation Experiment (LPVEx). These events have been simulated using the Weather Research and Forecasting Model coupled with spectral bin microphysics (WRF?SBM). The detailed ice-melting scheme with prognosis of the liquid water fraction during melting enables explicit simulation of microphysical properties in the melting layer. First, the simulations have been compared with C-band 3D radar measurements for the purpose of evaluating the overall profiles of cloud and precipitation. The simulation has some artificial convective patterns and errors in the forecast displacement of the precipitation system. The overall overestimation of reflectivity is consistent with a bias toward the range characterized by large-diameter droplets in the surface drop size distribution. Second, the structure of the melting bands has been evaluated against vertically pointing K-band radar measurements. A peak in reflectivity and a gradual change in Doppler velocity are observed and similarly simulated in the common temperature range from approximately 0° to 3°C. The effectiveness of the time-dependent melting scheme has been justified by intercomparison with a corresponding simulation using an instantaneous melting scheme. A weakness of the new melting scheme is that melting particles having high liquid water fractions on the order of 80%?90% cannot be simulated. This situation may cause underestimation of radar reflectivity in the melting layer because of the assumptions of melting-particle structure used to calculate the scattering properties.
    publisherAmerican Meteorological Society
    titleWRF–SBM Simulations of Melting-Layer Structure in Mixed-Phase Precipitation Events Observed during LPVEx
    typeJournal Paper
    journal volume53
    journal issue12
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-13-0334.1
    journal fristpage2710
    journal lastpage2731
    treeJournal of Applied Meteorology and Climatology:;2014:;volume( 053 ):;issue: 012
    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