HR: 0800h
AN: H11F-0382 [Abstracts]
TI: Potential Effects of Wildfire on Watershed Hydrologic Response: Sabino Creek Basin, Arizona
AU: * Guardiola-Claramonte, M
EM: maite@hwr.arizona.edu
AF: Hydrology and Water Resources, PO Box 210011
The University of Arizona, Tucson, AZ 85721-0011
United States
AU: Nijssen, B
EM: nijssen@u.arizona.edu
AF: Hydrology and Water Resources, PO Box 210011
The University of Arizona, Tucson, AZ 85721-0011
United States
AU: Nijssen, B
EM: nijssen@u.arizona.edu
AF: Civil Engineering and Engineering Mechanics, PO Box 210072
The University of Arizona, Tucson, AZ 85721-0072
United States
AB:
Wildfires and their hydrologic consequences, such as flash floods and mudslides, pose serious hazards in the southwestern
United States. As a result of the present drought and decades of fire suppression, wildfires are occurring with greater
frequency and intensity. Preservation or rehabilitation zones can be identified in a watershed to minimize the severity of
secondary-order fire effects, such as erosion, increased flow peaks and landslides. Distributed hydrological models can be a
useful tool to locate these zones. In this study, a distributed watershed model was used to evaluate the effects of pre- and
post-fire land use scenarios on watershed hydrologic response in the Sabino Creek watershed north of Tucson, Arizona. During
the summer of 2003, the Aspen fire burned in excess of 34 thousand hectares in the Santa Catalina Mountains, including a
large part of the study basin. To model the watershed, field and laboratory measurements of soil permeability in burned and
unburned areas were used, together with fifteen years of climatological data from NOAA, USGS and Pima County. To investigate
the hydrologic effects of wildfire, model simulations using pre- and post-fire soil and vegetation parameters, in particular
soil permeability and leaf area index, were compared to each other as well as to field observations.
DE: 1821 Floods
DE: 1836 Hydrologic budget (1655)
DE: 1860 Runoff and streamflow
SC: Hydrology [H]
MN: 2004 AGU Fall Meeting