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    Anchorage Windstorm of 1 December 1992

    Source: Weather and Forecasting:;1994:;volume( 009 ):;issue: 004::page 469
    Author:
    Hopkins, Robert H.
    DOI: 10.1175/1520-0434(1994)009<0469:AWOD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: On 1 December 1992 a strong downslope windstorm with an atypical damage pattern hit Anchorage. Downslope windstorms are common in Anchorage from September through April. Typically damaging winds from these storms are confined to the foothills of the Chugach Mountains and east Anchorage within 5 km of the edge of the foothills. In the 1 December storm, moderate wind damage occurred across the entire city in areas where wind damage is a rarity during downslope windstorms. Anchorage forecasters use an empirically derived automated technique to forecast downslope windstorms. The technique works very well. It is the purpose of this study to add to this technique so that atypical storms like the 1 December storm can be detected in advance. Historical records were searched and two storms with similar atypical damage patterns were found. In this study the 1 December windstorm is described, the two historical storms with similar atypical damage patterns are described, and a forecast tool is devised using a combination of characteristics common to the three storms that is hopefully unique. A by-product of this study is a synoptic-scale tool for forecasting the onset of maximum winds for the majority of Anchorage downslope windstorms.
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      Anchorage Windstorm of 1 December 1992

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4164512
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    contributor authorHopkins, Robert H.
    date accessioned2017-06-09T14:49:12Z
    date available2017-06-09T14:49:12Z
    date copyright1994/12/01
    date issued1994
    identifier issn0882-8156
    identifier otherams-2750.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164512
    description abstractOn 1 December 1992 a strong downslope windstorm with an atypical damage pattern hit Anchorage. Downslope windstorms are common in Anchorage from September through April. Typically damaging winds from these storms are confined to the foothills of the Chugach Mountains and east Anchorage within 5 km of the edge of the foothills. In the 1 December storm, moderate wind damage occurred across the entire city in areas where wind damage is a rarity during downslope windstorms. Anchorage forecasters use an empirically derived automated technique to forecast downslope windstorms. The technique works very well. It is the purpose of this study to add to this technique so that atypical storms like the 1 December storm can be detected in advance. Historical records were searched and two storms with similar atypical damage patterns were found. In this study the 1 December windstorm is described, the two historical storms with similar atypical damage patterns are described, and a forecast tool is devised using a combination of characteristics common to the three storms that is hopefully unique. A by-product of this study is a synoptic-scale tool for forecasting the onset of maximum winds for the majority of Anchorage downslope windstorms.
    publisherAmerican Meteorological Society
    titleAnchorage Windstorm of 1 December 1992
    typeJournal Paper
    journal volume9
    journal issue4
    journal titleWeather and Forecasting
    identifier doi10.1175/1520-0434(1994)009<0469:AWOD>2.0.CO;2
    journal fristpage469
    journal lastpage478
    treeWeather and Forecasting:;1994:;volume( 009 ):;issue: 004
    contenttypeFulltext
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