Streamflow levels across
Utah
are currently
128.0% of normal, with the
Green River At Mineral Bottom Nr Cynlnds Ntl Park
reporting the highest discharge in the state with
7700cfs and gauge stage of 11.1 ft.
Meanwhile, the
Sevier River Near Juab
is seeing a spike in streamflows today after experiencing a
104400.0%
increase since yesterday, and currently running at
209cfs.
Maximum gauge stage in the state was last observed at the
Santa Clara Riv Blw Winsor Dam, currently reporting a stage of
16.63ft.
The
Goggin Drain Near Magna Utah
in the
Jordan
watershed
is surging for this time of year at
1050cfs, about
334.96% of normal.
Surface Flow Characteristics
Utah has a semi-arid climate with variable precipitation patterns and significant snowfall in the mountains. Major surface flows include the Great Salt Lake, Utah Lake, and Bear Lake, with numerous reservoirs and dams throughout the state. The Colorado River and its tributaries, including the Green River, are vital sources of water for Utah. The state's hydrology is heavily influenced by its topography, with the Wasatch Mountains playing a key role in snowpack accumulation and runoff. The snowpack is critical for providing water to the state's major rivers and irrigation systems. Watershed data is closely monitored to predict and manage water availability in the state, with a focus on balancing agricultural, municipal, and environmental needs.
Streamgauge Profile
Statewide Warnings & Alerts
Rivers of Utah
Watersheds of Utah
Popular Whitewater Destinations
River Run | Status | Streamflow (CFS) | Air Temp (F) |
---|---|---|---|
|
TOO HIGH | 199 | 62 |
|
RUNNABLE | 1200 | 64 |
|
49.26 | ||
|
TOO HIGH | 1200 | 64 |
|
RUNNABLE | 3430 | 70 |
|
TOO HIGH | 340 | 63 |
|
RUNNABLE | 1200 | 64 |
|
TOO LOW | 128 | 66 |
|
65.7 | ||
|
TOO HIGH | 4620 | 77 |
|
55.09 | ||
|
TOO HIGH | 2600 | 83 |
|
RUNNABLE | 44.8 | 56 |
|
TOO LOW | 53.8 | 69 |
|
63.28 | ||
|
RUNNABLE | 0.77 | 68 |
|
TOO HIGH | 4620 | 77 |
|
RUNNABLE | 14.1 | 71 |
|
TOO HIGH | 2600 | 83 |
|
TOO LOW | 505 | 74 |
|
58.46 | ||
|
TOO HIGH | 127 | 64 |
|
TOO LOW | 153 | 61 |
|
TOO LOW | 505 | 74 |
|
RUNNABLE | 530 | 80 |
|
TOO HIGH | 239 | 60 |
|
TOO HIGH | 4620 | 77 |
|
RUNNABLE | 0.77 | 68 |
|
RUNNABLE | 0.77 | 68 |
|
47.07 | ||
|
TOO LOW | 59.5 | 82 |
|
RUNNABLE | 153 | 61 |
|
TOO HIGH | 324 | 71 |
|
RUNNABLE | 888 | 60 |
|
TOO HIGH | 92.3 | 73 |
|
57.18 | ||
|
52.11 | ||
|
RUNNABLE | 153 | 61 |
|
TOO HIGH | 127 | 64 |
|
TOO LOW | 0.77 | 68 |
|
RUNNABLE | 0.77 | 68 |
|
RUNNABLE | 530 | 80 |
|
47.46 | ||
|
TOO HIGH | 308 | 69 |
|
RUNNABLE | 31.9 | 67 |
|
TOO HIGH | 11.7 | 62 |
|
RUNNABLE | 76.1 | 67 |
|
RUNNABLE | 148 | 71 |
|
RUNNABLE | 888 | 60 |
|
RUNNABLE | 888 | 60 |
|
TOO HIGH | 127 | 64 |
|
RUNNABLE | 155 | 58 |
|
RUNNABLE | 888 | 60 |
The Chute - Tomsich Butte to Hidden Splender
Class II to II+ |
RUNNABLE | 14.1 | 71 |
|
52.43 | ||
|
TOO LOW | 59.5 | 82 |
|
TOO HIGH | 59.6 | 62 |
|
TOO HIGH | 59.6 | 62 |
|
TOO HIGH | 59.6 | 62 |
|
RUNNABLE | 239 | 60 |
|
RUNNABLE | 239 | 60 |
|
TOO LOW | 59.5 | 82 |
|
56.41 | ||
|
RUNNABLE | 44.8 | 56 |
|
TOO HIGH | 4620 | 77 |
|
60.89 | ||
|
RUNNABLE | 61.8 | 64 |
|
RUNNABLE | 61.8 | 64 |
|
TOO LOW | 93.8 | 83 |