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    Changes in the Timing of Snowmelt and Streamflow in Colorado: A Response to Recent Warming

    Source: Journal of Climate:;2009:;volume( 023 ):;issue: 009::page 2293
    Author:
    Clow, David W.
    DOI: 10.1175/2009JCLI2951.1
    Publisher: American Meteorological Society
    Abstract: Trends in the timing of snowmelt and associated runoff in Colorado were evaluated for the 1978?2007 water years using the regional Kendall test (RKT) on daily snow-water equivalent (SWE) data from snowpack telemetry (SNOTEL) sites and daily streamflow data from headwater streams. The RKT is a robust, nonparametric test that provides an increased power of trend detection by grouping data from multiple sites within a given geographic region. The RKT analyses indicated strong, pervasive trends in snowmelt and streamflow timing, which have shifted toward earlier in the year by a median of 2?3 weeks over the 29-yr study period. In contrast, relatively few statistically significant trends were detected using simple linear regression. RKT analyses also indicated that November?May air temperatures increased by a median of 0.9°C decade?1, while 1 April SWE and maximum SWE declined by a median of 4.1 and 3.6 cm decade?1, respectively. Multiple linear regression models were created, using monthly air temperatures, snowfall, latitude, and elevation as explanatory variables to identify major controlling factors on snowmelt timing. The models accounted for 45% of the variance in snowmelt onset, and 78% of the variance in the snowmelt center of mass (when half the snowpack had melted). Variations in springtime air temperature and SWE explained most of the interannual variability in snowmelt timing. Regression coefficients for air temperature were negative, indicating that warm temperatures promote early melt. Regression coefficients for SWE, latitude, and elevation were positive, indicating that abundant snowfall tends to delay snowmelt, and snowmelt tends to occur later at northern latitudes and high elevations. Results from this study indicate that even the mountains of Colorado, with their high elevations and cold snowpacks, are experiencing substantial shifts in the timing of snowmelt and snowmelt runoff toward earlier in the year.
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      Changes in the Timing of Snowmelt and Streamflow in Colorado: A Response to Recent Warming

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    contributor authorClow, David W.
    date accessioned2017-06-09T16:29:28Z
    date available2017-06-09T16:29:28Z
    date copyright2010/05/01
    date issued2009
    identifier issn0894-8755
    identifier otherams-68816.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210416
    description abstractTrends in the timing of snowmelt and associated runoff in Colorado were evaluated for the 1978?2007 water years using the regional Kendall test (RKT) on daily snow-water equivalent (SWE) data from snowpack telemetry (SNOTEL) sites and daily streamflow data from headwater streams. The RKT is a robust, nonparametric test that provides an increased power of trend detection by grouping data from multiple sites within a given geographic region. The RKT analyses indicated strong, pervasive trends in snowmelt and streamflow timing, which have shifted toward earlier in the year by a median of 2?3 weeks over the 29-yr study period. In contrast, relatively few statistically significant trends were detected using simple linear regression. RKT analyses also indicated that November?May air temperatures increased by a median of 0.9°C decade?1, while 1 April SWE and maximum SWE declined by a median of 4.1 and 3.6 cm decade?1, respectively. Multiple linear regression models were created, using monthly air temperatures, snowfall, latitude, and elevation as explanatory variables to identify major controlling factors on snowmelt timing. The models accounted for 45% of the variance in snowmelt onset, and 78% of the variance in the snowmelt center of mass (when half the snowpack had melted). Variations in springtime air temperature and SWE explained most of the interannual variability in snowmelt timing. Regression coefficients for air temperature were negative, indicating that warm temperatures promote early melt. Regression coefficients for SWE, latitude, and elevation were positive, indicating that abundant snowfall tends to delay snowmelt, and snowmelt tends to occur later at northern latitudes and high elevations. Results from this study indicate that even the mountains of Colorado, with their high elevations and cold snowpacks, are experiencing substantial shifts in the timing of snowmelt and snowmelt runoff toward earlier in the year.
    publisherAmerican Meteorological Society
    titleChanges in the Timing of Snowmelt and Streamflow in Colorado: A Response to Recent Warming
    typeJournal Paper
    journal volume23
    journal issue9
    journal titleJournal of Climate
    identifier doi10.1175/2009JCLI2951.1
    journal fristpage2293
    journal lastpage2306
    treeJournal of Climate:;2009:;volume( 023 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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