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Cory Miller
Student Watershed Research Award Recipient
Graduate Student
School of Forestry and Ecological Restoration Institute
cory.miller@nau.edu

c.miller@landterms.com

Advisor: Dr. Wallace Covington

Analysis of Current and Historical Surface Flows and Hydrologic Response to Restoration Treatments in the Upper Lake Mary Watershed, Arizona

Upper Lake Mary is the sole surface water reservoir for Flagstaff, Arizona, and has historically provided 40% of the city’s drinking water.  The forested watershed has grown dense with trees since large-scale logging, livestock grazing, and fire suppression activities began approximately 135 years ago.  Surface flows into the reservoir have declined over time, even in years with similar precipitation.  These factors suggest that a likely cause is the increased transpiration and interception of precipitation that accompanies increased overstory vegetation.  In its current condition, the watershed is at risk for severe wildfire that could impede its ability to meet water quality standards for domestic purposes.  This study was undertaken to assess forest management solutions to these problems.  We calculated current and historic surface flows based on forest inventory results.  Four management alternatives were analyzed: no action, thinning to 75% of current basal area, thinning to 50% of current basal area, and restoration treatments based on historic reference conditions.  We modeled water yields, sedimentation, and erosion resulting from these treatments.  We also determined the possible effects of severe wildfire on sedimentation, erosion, and water quality.  Water yield increases ranged from 3%-6.6% for thinning to 75% of current basal area, 10.5%-19% for 50% reduction, and 17%-28.9% for ecological restoration treatments.  Restoration treatment values are also the approximate amounts by which streamflows have declined since about 1870.  Erosion soil loss tolerances were exceeded in the wildfire scenario, and for ecological restoration treatments in some areas greater than 15% slope, but only in the first few years following disturbance.  Of the three thinning alternatives modeled, only restoration treatments were self-sustaining in terms of maintenance and renewal of streamflow response, because of re-introduction of a frequent, low-intensity fire regime.

Cory Miller's Master's Project Professional Paper (6.5MB PDF) 

 

 
 

 
Watershed Research & Education Program
Department of Civil & Environmental Engineering
Northern Arizona University
PO Box 15600
Flagstaff, AZ 86011