Last Updated: January 1, 2026
As we examine the current state of Arizona's river systems, we find a mix of streamflow conditions, with several waterways experiencing lower-than-normal flows. Enthusiasts and professionals should note that the Colorado River at Lees Ferry, a critical point for water resource management, shows a current streamflow of 7,570 cubic feet per second (cfs), which is a notable 38.96% below its typical flow for this time of year. This trend of reduced flow continues at other locations along the Colorado River, including near the Grand Canyon and above Diamond Creek near Peach Springs, with flows at 73.45% and 76.16% of their normal levels, respectively. Such declines could impact recreational activities and ecosystems reliant on steady flows.
In contrast, the Virgin River at Littlefield and above The Narrows near Littlefield is flowing at 77.76% and 96.78% of the expected volume, suggesting healthier conditions for local water sports. However, the Gila River at the head of Safford Valley and the Salt River near Roosevelt are experiencing significant flow deficits, operating at 43.19% and 41.26% of normal, which may indicate flow droughts affecting those watersheds. The Verde River, with locations near Scottsdale and below Bartlett Dam, has also seen substantial 24-hour decreases in flow, dropping by 38.24 cfs and 46.48 cfs, respectively, though they remain closer to normal levels. These dramatic changes in streamflow could suggest potential for drought or, with rapid increases, risks of flooding that could influence the surrounding communities and riparian habitats. Water enthusiasts, particularly those interested in whitewater trails in the Salt River Canyon or along the Verde River, should remain vigilant to these fluctuations for planning and safety considerations.
Arizona is a state with arid to semi-arid climate conditions. Major surface flows include the Colorado and Gila Rivers, with the former having significant impacts on water supply and hydroelectricity generation. Reservoirs and dams, such as Lake Powell and Hoover Dam, play critical roles in water storage and management. The state's hydrology is primarily influenced by snowmelt from the Rocky Mountains and the monsoon season, which brings heavy rainfall to the region during the summer months. Watershed data indicates that the Salt and Verde Rivers are the primary sources of water for the Phoenix metropolitan area. Climate change is expected to exacerbate water scarcity issues in the region, with reduced snowpack and increased temperatures leading to higher evaporation rates and reduced water availability.
| River Run | Status | Streamflow (CFS) | Air Temp (F) |
|---|---|---|---|
|
Christopher Creek
Class V |
TOO HIGH | 443 | 83 |
|
Christopher Creek
Class V |
TOO HIGH | 443 | 83 |
|
Christopher Creek
Class V |
TOO HIGH | 443 | 83 |
|
Grand Canyon
Class III to IV |
RUNNABLE | 9320 | 82 |
|
Hell's Gate Canyon
Class V |
TOO LOW | 14.9 | 81 |
|
Indian Gardens
Class IV- to IV+ |
TOO LOW | 30.4 | 76 |
|
Kelvin Run
Class I to II- |
73.27 | ||
|
Lower Salt
Class I |
RUNNABLE | 575 | 90 |
|
Lower Verde
Class I to II |
RUNNABLE | 127 | 88 |
|
Upper Salt Daily
Class III to IV |
67.33 | ||
|
White Bridge to Beasley Flat
Class II- to II |
65.68 |