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    • Hydrology and Water Resources in Arizona and the Southwest, Volume 02 (1972)
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    An Analysis of Yearly Differences in Snowpack Inventory-Prediction Relationships

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    Author
    Ffolliott, Peter F.
    Thorud, David B.
    Enz, Richard W.
    Affiliation
    Department of Watershed Management, University of Arizona, Tucson 85721
    USDA Soil Conservation Service, Phoenix, Arizona 85025
    Issue Date
    1972-05-06
    Keywords
    Hydrology -- Arizona.
    Water resources development -- Arizona.
    Hydrology -- Southwestern states.
    Water resources development -- Southwestern states.
    Runoff forecasting
    Snowpacks
    Spatial distribution
    Forest management
    Vegetation effects
    Arizona
    Forecasting
    Census
    Forests
    Watershed management
    Snow surveys
    Water equivalent
    Water yield
    Snow management
    Canopy
    Inventory-prediction
    Ponderosa pine
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    Copyright ©, where appropriate, is held by the author.
    Collection Information
    This article is part of the Hydrology and Water Resources in Arizona and the Southwest collections. Digital access to this material is made possible by the Arizona-Nevada Academy of Science and the University of Arizona Libraries. For more information about items in this collection, contact anashydrology@gmail.com.
    Publisher
    Arizona-Nevada Academy of Science
    Journal
    Hydrology and Water Resources in Arizona and the Southwest
    Abstract
    Inventory-prediction relationships between snowpack conditions and forest attributes may be useful in estimating water yields derived from snow, but such relationships are developed usually from source data collected over a short time period. Analyses of long-term data suggest inventory-prediction relationships developed from limited data may have more general application, however. Available records from 18 snow courses in the ponderosa pine type in Arizona provided source data in this study, which was designed to empirically analyze inventory-prediction relationships developed from long-term snow survey records. The primary hypothesis tested and evaluated by statistically analyzing the family of regression equations representing a snow course, was that, given a precipitation input, the distribution of snowpack water equivalent at peak seasonal accumulation is determined by the spatial arrangement of the forest cover, e.g. basal area. Generally 12 of the 18 snow courses evaluated appeared to support the hypothesis, three courses did not, and three courses were considered inconclusive.
    ISSN
    0272-6106
    Collections
    Hydrology and Water Resources in Arizona and the Southwest, Volume 02 (1972)

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