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    Characteristics of Sonoran Desert Microbursts

    Source: Weather and Forecasting:;2010:;volume( 026 ):;issue: 001::page 94
    Author:
    Willingham, Katherine M.
    ,
    Thompson, Elizabeth J.
    ,
    Howard, Kenneth W.
    ,
    Dempsey, Charles L.
    DOI: 10.1175/2010WAF2222388.1
    Publisher: American Meteorological Society
    Abstract: During the 2008 North American monsoon season, 140 microburst events were identified in Phoenix, Arizona, and the surrounding Sonoran Desert. The Sonoran microbursts were studied and examined for their frequency and characteristics, as observed from data collected from three Doppler radars and electrical power infrastructure damage reports. Sonoran microburst events were wet microbursts and occurred most frequently in the evening hours (1900?2100 local time). Stronger maximum differential velocities (20?25 m s?1) were observed more frequently in Sonoran microbursts than in many previously documented microbursts. Alignment of Doppler radar data to reports of wind-related damage to electrical power infrastructure in Phoenix allowed a comparison of microburst wind damage versus gust-front wind damage. For these damage reports, microburst winds caused more significant damage than gust-front winds.
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      Characteristics of Sonoran Desert Microbursts

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4213384
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    contributor authorWillingham, Katherine M.
    contributor authorThompson, Elizabeth J.
    contributor authorHoward, Kenneth W.
    contributor authorDempsey, Charles L.
    date accessioned2017-06-09T16:38:44Z
    date available2017-06-09T16:38:44Z
    date copyright2011/02/01
    date issued2010
    identifier issn0882-8156
    identifier otherams-71487.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4213384
    description abstractDuring the 2008 North American monsoon season, 140 microburst events were identified in Phoenix, Arizona, and the surrounding Sonoran Desert. The Sonoran microbursts were studied and examined for their frequency and characteristics, as observed from data collected from three Doppler radars and electrical power infrastructure damage reports. Sonoran microburst events were wet microbursts and occurred most frequently in the evening hours (1900?2100 local time). Stronger maximum differential velocities (20?25 m s?1) were observed more frequently in Sonoran microbursts than in many previously documented microbursts. Alignment of Doppler radar data to reports of wind-related damage to electrical power infrastructure in Phoenix allowed a comparison of microburst wind damage versus gust-front wind damage. For these damage reports, microburst winds caused more significant damage than gust-front winds.
    publisherAmerican Meteorological Society
    titleCharacteristics of Sonoran Desert Microbursts
    typeJournal Paper
    journal volume26
    journal issue1
    journal titleWeather and Forecasting
    identifier doi10.1175/2010WAF2222388.1
    journal fristpage94
    journal lastpage108
    treeWeather and Forecasting:;2010:;volume( 026 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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