Last Updated: December 4, 2025
In Arizona, the Colorado River system, significant for its life-sustaining water supply and recreational opportunities, displays varied streamflow conditions, crucial for enthusiasts tracking seasonal trends and potential water-related events. The Colorado River at Lees Ferry, a key location for water allocation and management, is currently flowing at 8,810 cubic feet per second (cfs), which is 29.55% below normal, indicating a period of lower than average flow, important for users to note. Similarly, upstream and downstream points, such as near Grand Canyon and above Diamond Creek near Peach Springs, show decreased flows at 7,650 cfs and 9,430 cfs, 28.32% and 15.3% below normal, respectively, which could affect both ecosystems and river recreation.
Local river systems also demonstrate noteworthy conditions; the Verde River, critical for central Arizona's water supply and a popular recreation site near Scottsdale, flows at a reduced rate of 152 cfs, 48.88% below normal, potentially impacting local water availability and stream activities. In contrast, the East Verde River near Childs remarkably exceeds its average at 133 cfs, an astounding 408.8% of normal, raising attention to the possibility of flooding or enhanced recreational flows. The Salt River, a source of Phoenix's water and a favorite among whitewater enthusiasts, shows varied streamflow along its course, with the point below Stewart Mountain Dam notably at 198 cfs, 71.62% above normal, suggesting conditions favorable for water activities but warranting vigilance for potential stream level increases. These streamflow variations across Arizona's river systems highlight the need for continuous monitoring to assure water resource management, recreational safety, and ecological health.
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 |