IDAHO FLOW REPORT

Last Updated: December 28, 2025

Idaho's streamflow conditions reflect a diverse hydrological landscape with several rivers experiencing significant fluctuations in water levels. Currently, many rivers are reporting below-normal streamflows, such as the Henrys Fork near Island Park with only 203 cubic feet per second (cfs), which is 38.5% below normal, and the Snake River near Irwin flowing at 925 cfs, 19.94% below normal. Contrarily, the South Fork of the Coeur d'Alene River near Pinehurst stands out at 785 cfs, marking an impressive 169.82% of its normal flow. Water enthusiasts and communities should note that the Kootenai River at Porthill reports a substantial flow of 26,900 cfs, although it is 51.16% of the normal volume, which could impact local areas, including the city of Bonners Ferry.

Anomalies such as the Boundary Creek near Porthill, flowing at 281 cfs or 177.53% of the normal, may interest whitewater enthusiasts for potential recreational opportunities, given the high percentage of normal flow. In contrast, regions such as Twin Falls could experience stress on water resources, with the Snake River near Twin Falls flowing at 676 cfs, 44.19% below normal. The varying conditions across the state, including potential flooding areas like the Boise River at Caldwell flowing at 558 cfs, or drought-like conditions in other regions, highlight the importance of continuous monitoring and adaptive water management strategies for Idaho's rivers and watersheds.

       



Idaho's flow conditions are influenced by its unique hydrology and climate characteristics. The state has numerous major surface flows, including the Snake River, Salmon River, and Clearwater River, all of which are important for irrigation, hydroelectric power, and recreation. Idaho also has several large reservoirs and dams, such as the Boise River Reservoir and Lucky Peak Dam, which play a crucial role in regulating water flow and supply. The state's watersheds and snowpack levels are also significant indicators of hydrologic conditions, with winter snowpack providing a critical source of water for the state's rivers and streams during the summer months. Overall, Idaho's flow conditions are shaped by a complex interplay of natural and human factors, making it an important area of study for hydrologists and water resource managers.


       

Rafting & Kayaking

River Run Status Streamflow (CFS) Air Temp (F)
32nd Street to Smelter
Class III to IV-
34.11
TOO HIGH 1630 59
RUNNABLE 144 56
RUNNABLE 3670 48
RUNNABLE 3670 48
RUNNABLE 3670 48
RUNNABLE 3670 48
RUNNABLE 3670 48
Box Canyon
Class II
RUNNABLE 267 50
RUNNABLE 1270 53
Cabarton
Class II to III
TOO LOW 44.6 35
RUNNABLE 1070 55
Coffee Pot
Class III
RUNNABLE 390 48
TOO HIGH 1070 55
RUNNABLE 1560 54
RUNNABLE 1560 54
RUNNABLE 1560 54
RUNNABLE 1070 55
RUNNABLE 2490 58
35.94
TOO LOW 527 58
TOO HIGH 1070 55
RUNNABLE 9860 51
216 45
Murphy to Bruneau
Class III- to V
TOO LOW 20 57
Murphy to Bruneau
Class III- to V
TOO LOW 20 57
Murphy to Bruneau
Class III- to V
TOO LOW 20 57
TOO LOW 57
Pahsimeroi to Royal Gorge
Class II- to III-
TOO HIGH 1070 55
RUNNABLE 3090 45
42.37
35.55
RUNNABLE 9860 51
TOO HIGH 1070 55
418 49
Split Creek to Lowell
Class II+ to III+
RUNNABLE 2490 58
TOO HIGH 1070 55
RUNNABLE 1070 55
RUNNABLE 2490 58
42.12