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    A Climatology of Snow-to-Liquid Ratio for the Contiguous United States

    Source: Weather and Forecasting:;2005:;volume( 020 ):;issue: 005::page 729
    Author:
    Baxter, Martin A.
    ,
    Graves, Charles E.
    ,
    Moore, James T.
    DOI: 10.1175/WAF856.1
    Publisher: American Meteorological Society
    Abstract: A 30-yr climatology of the snow-to-liquid-equivalent ratio (SLR) using the National Weather Service (NWS) Cooperative Summary of the Day (COOP) data is presented. Descriptive statistics are presented for 96 NWS county warning areas (CWAs), along with a discussion of selected histograms of interest. The results of the climatology indicate that a mean SLR value of 13 appears more appropriate for much of the country rather than the often-assumed value of 10, although considerable spatial variation in the mean exists. The distribution for the entire dataset exhibits positive skewness. Histograms for individual CWAs are both positively and negatively skewed, depending upon the variability of the in-cloud, subcloud, and ground conditions.
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      A Climatology of Snow-to-Liquid Ratio for the Contiguous United States

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4231221
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    contributor authorBaxter, Martin A.
    contributor authorGraves, Charles E.
    contributor authorMoore, James T.
    date accessioned2017-06-09T17:34:56Z
    date available2017-06-09T17:34:56Z
    date copyright2005/10/01
    date issued2005
    identifier issn0882-8156
    identifier otherams-87541.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4231221
    description abstractA 30-yr climatology of the snow-to-liquid-equivalent ratio (SLR) using the National Weather Service (NWS) Cooperative Summary of the Day (COOP) data is presented. Descriptive statistics are presented for 96 NWS county warning areas (CWAs), along with a discussion of selected histograms of interest. The results of the climatology indicate that a mean SLR value of 13 appears more appropriate for much of the country rather than the often-assumed value of 10, although considerable spatial variation in the mean exists. The distribution for the entire dataset exhibits positive skewness. Histograms for individual CWAs are both positively and negatively skewed, depending upon the variability of the in-cloud, subcloud, and ground conditions.
    publisherAmerican Meteorological Society
    titleA Climatology of Snow-to-Liquid Ratio for the Contiguous United States
    typeJournal Paper
    journal volume20
    journal issue5
    journal titleWeather and Forecasting
    identifier doi10.1175/WAF856.1
    journal fristpage729
    journal lastpage744
    treeWeather and Forecasting:;2005:;volume( 020 ):;issue: 005
    contenttypeFulltext
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