Research conducted on burned watersheds throughout the Rockies indicates hydrologic recovery to near pre-burn conditions within 3 to 5 years. This study looks at hydrologic recovery for a small basin in southern Arizona (Figure 1). Two significant flow events are studied in the Campo Bonito watershed. The initial event occurred during the summer immediately following the fires. This event was first documented in National Weather Service (NWS) Western Region Technical Attachment 03-10 (Schaffner 2003). The second event occurred two years later in 2005. This work builds upon the 2003 technical attachment. Improvements include GIS analysis of burn severity, a more detailed look at ...
This research investigates the impact of wildfires on watershed flow regimes, specifically focusing...
Debris flows in a burned area, post-fire debris flows, are considered as one of the most dangerous g...
Erosion and runoff have been observed to increase following fire. Land managers and Burned Area Emer...
In the desert southwest of the United States, wildfire alters the hydrologic response o...
This updated study focused on the methodologies, tools, and applications used to evaluate the hydrol...
This paper documents the hydrologic response of nine watersheds in Southeast Arizona within the firs...
From the Proceedings of the 1985 Meetings of the Arizona Section - American Water Resources Associat...
Extreme floods often follow wildfire in mountainous watersheds. However, a quantitative relation bet...
Trends of increasing wildfire size and severity across the western U.S. and concurrent encroachment ...
As a result of drought and decades of fire suppression, wildfires are occurring with greater frequen...
Fire on rangelands used as a management tool or as an unwanted wildfire removes vegetation cover. Ve...
This paper presents the new fundamental concept of the hyper-effective drainage area, the area of th...
In June, 2010, the human-caused Schultz Fire near Flagstaff burned 6,100 ha of mostly steep terrain....
The Coon Creek Wildfire in 2000 and the Rodeo-Chediski Wildfire in 2002 devastated large areas of fo...
Wildfires alter land surfaces and land-atmosphere interactions, causing enhanced runoff and debris f...
This research investigates the impact of wildfires on watershed flow regimes, specifically focusing...
Debris flows in a burned area, post-fire debris flows, are considered as one of the most dangerous g...
Erosion and runoff have been observed to increase following fire. Land managers and Burned Area Emer...
In the desert southwest of the United States, wildfire alters the hydrologic response o...
This updated study focused on the methodologies, tools, and applications used to evaluate the hydrol...
This paper documents the hydrologic response of nine watersheds in Southeast Arizona within the firs...
From the Proceedings of the 1985 Meetings of the Arizona Section - American Water Resources Associat...
Extreme floods often follow wildfire in mountainous watersheds. However, a quantitative relation bet...
Trends of increasing wildfire size and severity across the western U.S. and concurrent encroachment ...
As a result of drought and decades of fire suppression, wildfires are occurring with greater frequen...
Fire on rangelands used as a management tool or as an unwanted wildfire removes vegetation cover. Ve...
This paper presents the new fundamental concept of the hyper-effective drainage area, the area of th...
In June, 2010, the human-caused Schultz Fire near Flagstaff burned 6,100 ha of mostly steep terrain....
The Coon Creek Wildfire in 2000 and the Rodeo-Chediski Wildfire in 2002 devastated large areas of fo...
Wildfires alter land surfaces and land-atmosphere interactions, causing enhanced runoff and debris f...
This research investigates the impact of wildfires on watershed flow regimes, specifically focusing...
Debris flows in a burned area, post-fire debris flows, are considered as one of the most dangerous g...
Erosion and runoff have been observed to increase following fire. Land managers and Burned Area Emer...