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    Hydrologic Visibility of Weather Radar Systems Operating in Mountainous Regions: Case Study for the Ardèche Catchment (France)

    Source: Journal of Hydrometeorology:;2002:;Volume( 003 ):;issue: 005::page 539
    Author:
    Pellarin, Thierry
    ,
    Delrieu, Guy
    ,
    Saulnier, Georges-Marie
    ,
    Andrieu, Hervé
    ,
    Vignal, Bertrand
    ,
    Creutin, Jean-Dominique
    DOI: 10.1175/1525-7541(2002)003<0539:HVOWRS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A simulation procedure has been developed for use in predetermining the expected quality of rain-rate estimates that a given weather radar system operating in a mountainous region may obtain over a given hydrologic catchment. This first application of what is referred to as the ?hydrologic visibility? concept focuses on the quantification of the rain-rate error resulting from the effects of ground clutter, beam blockage, and the vertical profile of reflectivity (VPR). The assessment of the impact of the space?time structure of the radar error in terms of discharge at the catchment outlet is also investigated using a distributed hydrologic model. A case study is presented for the Ardèche catchment in France using the parameters of two S-band weather radars operated by Météo-France at Nîmes and Bollène. Radar rain-rate error generation and rainfall?runoff simulations are performed using VPR and areal rainfall time series representative of the Cévennes rain climatology. The major impact of ground clutter on both rainfall and runoff estimates is confirmed. The ?hydrologic compositing procedure,? based on the selection of the elevation angle minimizing the rain-rate error at a given point, is shown to be preferable to the ?pseudo-CAPPI? procedure based on radar-range considerations only. An almost perfect ground-clutter reduction (GCR) technique is simulated in order to assess the effects of beam blockage and VPR alone. These error sources lead to severe and slight rain underestimations for the Nîmes and Bollène radars, respectively, over the Ardèche catchment. The results, indicating an amplification of the errors on the discharge parameters (peak discharge, runoff volume) compared to the areal rainfall error, are of particular interest. They emphasize the need for refined corrections for ground clutter, beam blockage, and VPR effects, in addition to the optimization of the radar location and scanning strategy, if hydrologic applications are foreseen.
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      Hydrologic Visibility of Weather Radar Systems Operating in Mountainous Regions: Case Study for the Ardèche Catchment (France)

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4206233
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    • Journal of Hydrometeorology

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    contributor authorPellarin, Thierry
    contributor authorDelrieu, Guy
    contributor authorSaulnier, Georges-Marie
    contributor authorAndrieu, Hervé
    contributor authorVignal, Bertrand
    contributor authorCreutin, Jean-Dominique
    date accessioned2017-06-09T16:17:16Z
    date available2017-06-09T16:17:16Z
    date copyright2002/10/01
    date issued2002
    identifier issn1525-755X
    identifier otherams-65051.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206233
    description abstractA simulation procedure has been developed for use in predetermining the expected quality of rain-rate estimates that a given weather radar system operating in a mountainous region may obtain over a given hydrologic catchment. This first application of what is referred to as the ?hydrologic visibility? concept focuses on the quantification of the rain-rate error resulting from the effects of ground clutter, beam blockage, and the vertical profile of reflectivity (VPR). The assessment of the impact of the space?time structure of the radar error in terms of discharge at the catchment outlet is also investigated using a distributed hydrologic model. A case study is presented for the Ardèche catchment in France using the parameters of two S-band weather radars operated by Météo-France at Nîmes and Bollène. Radar rain-rate error generation and rainfall?runoff simulations are performed using VPR and areal rainfall time series representative of the Cévennes rain climatology. The major impact of ground clutter on both rainfall and runoff estimates is confirmed. The ?hydrologic compositing procedure,? based on the selection of the elevation angle minimizing the rain-rate error at a given point, is shown to be preferable to the ?pseudo-CAPPI? procedure based on radar-range considerations only. An almost perfect ground-clutter reduction (GCR) technique is simulated in order to assess the effects of beam blockage and VPR alone. These error sources lead to severe and slight rain underestimations for the Nîmes and Bollène radars, respectively, over the Ardèche catchment. The results, indicating an amplification of the errors on the discharge parameters (peak discharge, runoff volume) compared to the areal rainfall error, are of particular interest. They emphasize the need for refined corrections for ground clutter, beam blockage, and VPR effects, in addition to the optimization of the radar location and scanning strategy, if hydrologic applications are foreseen.
    publisherAmerican Meteorological Society
    titleHydrologic Visibility of Weather Radar Systems Operating in Mountainous Regions: Case Study for the Ardèche Catchment (France)
    typeJournal Paper
    journal volume3
    journal issue5
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/1525-7541(2002)003<0539:HVOWRS>2.0.CO;2
    journal fristpage539
    journal lastpage555
    treeJournal of Hydrometeorology:;2002:;Volume( 003 ):;issue: 005
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
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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