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    Value of a Dual-Polarized Gap-Filling Radar in Support of Southern California Post-Fire Debris-Flow Warnings

    Source: Journal of Hydrometeorology:;2011:;Volume( 012 ):;issue: 006::page 1581
    Author:
    Jorgensen, David P.
    ,
    Hanshaw, Maiana N.
    ,
    Schmidt, Kevin M.
    ,
    Laber, Jayme L.
    ,
    Staley, Dennis M.
    ,
    Kean, Jason W.
    ,
    Restrepo, Pedro J.
    DOI: 10.1175/JHM-D-11-05.1
    Publisher: American Meteorological Society
    Abstract: portable truck-mounted C-band Doppler weather radar was deployed to observe rainfall over the Station Fire burn area near Los Angeles, California, during the winter of 2009/10 to assist with debris-flow warning decisions. The deployments were a component of a joint NOAA?U.S. Geological Survey (USGS) research effort to improve definition of the rainfall conditions that trigger debris flows from steep topography within recent wildfire burn areas. A procedure was implemented to blend various dual-polarized estimators of precipitation (for radar observations taken below the freezing level) using threshold values for differential reflectivity and specific differential phase shift that improves the accuracy of the rainfall estimates over a specific burn area sited with terrestrial tipping-bucket rain gauges. The portable radar outperformed local Weather Surveillance Radar-1988 Doppler (WSR-88D) National Weather Service network radars in detecting rainfall capable of initiating post-fire runoff-generated debris flows. The network radars underestimated hourly precipitation totals by about 50%. Consistent with intensity?duration threshold curves determined from past debris-flow events in burned areas in Southern California, the portable radar-derived rainfall rates exceeded the empirical thresholds over a wider range of storm durations with a higher spatial resolution than local National Weather Service operational radars. Moreover, the truck-mounted C-band radar dual-polarimetric-derived estimates of rainfall intensity provided a better guide to the expected severity of debris-flow events, based on criteria derived from previous events using rain gauge data, than traditional radar-derived rainfall approaches using reflectivity?rainfall relationships for either the portable or operational network WSR-88D radars. Part of the reason for the improvement was due to siting the radar closer to the burn zone than the WSR-88Ds, but use of the dual-polarimetric variables improved the rainfall estimation by ~12% over the use of traditional Z?R relationships.
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      Value of a Dual-Polarized Gap-Filling Radar in Support of Southern California Post-Fire Debris-Flow Warnings

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4224768
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    • Journal of Hydrometeorology

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    contributor authorJorgensen, David P.
    contributor authorHanshaw, Maiana N.
    contributor authorSchmidt, Kevin M.
    contributor authorLaber, Jayme L.
    contributor authorStaley, Dennis M.
    contributor authorKean, Jason W.
    contributor authorRestrepo, Pedro J.
    date accessioned2017-06-09T17:14:41Z
    date available2017-06-09T17:14:41Z
    date copyright2011/12/01
    date issued2011
    identifier issn1525-755X
    identifier otherams-81732.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4224768
    description abstractportable truck-mounted C-band Doppler weather radar was deployed to observe rainfall over the Station Fire burn area near Los Angeles, California, during the winter of 2009/10 to assist with debris-flow warning decisions. The deployments were a component of a joint NOAA?U.S. Geological Survey (USGS) research effort to improve definition of the rainfall conditions that trigger debris flows from steep topography within recent wildfire burn areas. A procedure was implemented to blend various dual-polarized estimators of precipitation (for radar observations taken below the freezing level) using threshold values for differential reflectivity and specific differential phase shift that improves the accuracy of the rainfall estimates over a specific burn area sited with terrestrial tipping-bucket rain gauges. The portable radar outperformed local Weather Surveillance Radar-1988 Doppler (WSR-88D) National Weather Service network radars in detecting rainfall capable of initiating post-fire runoff-generated debris flows. The network radars underestimated hourly precipitation totals by about 50%. Consistent with intensity?duration threshold curves determined from past debris-flow events in burned areas in Southern California, the portable radar-derived rainfall rates exceeded the empirical thresholds over a wider range of storm durations with a higher spatial resolution than local National Weather Service operational radars. Moreover, the truck-mounted C-band radar dual-polarimetric-derived estimates of rainfall intensity provided a better guide to the expected severity of debris-flow events, based on criteria derived from previous events using rain gauge data, than traditional radar-derived rainfall approaches using reflectivity?rainfall relationships for either the portable or operational network WSR-88D radars. Part of the reason for the improvement was due to siting the radar closer to the burn zone than the WSR-88Ds, but use of the dual-polarimetric variables improved the rainfall estimation by ~12% over the use of traditional Z?R relationships.
    publisherAmerican Meteorological Society
    titleValue of a Dual-Polarized Gap-Filling Radar in Support of Southern California Post-Fire Debris-Flow Warnings
    typeJournal Paper
    journal volume12
    journal issue6
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM-D-11-05.1
    journal fristpage1581
    journal lastpage1595
    treeJournal of Hydrometeorology:;2011:;Volume( 012 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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