IDAHO FLOW REPORT

Last Updated: January 2, 2026

Idaho's rivers exhibit a variety of streamflow conditions, with several areas experiencing notable trends that are important for river enthusiasts and local communities. The Kootenai River at Leonia currently shows a significant streamflow at 25,300 cubic feet per second (cfs), which is above normal by 117.56%, indicating high water levels that could interest whitewater adventurers but also pose flooding risks. Contrastingly, the Snake River near Irwin is flowing at 912 cfs, 21.28% below the typical, suggesting a flow drought that could affect recreational activities and water availability. Similarly, the Falls River near Chester is substantially below normal at 48.17%, with only 542 cfs. In the Boise River Basin, flows near Caldwell indicate a slight decrease from the norm at 572 cfs.

Significant changes in streamflow have been observed in places such as the Blackfoot River near Shelley, with an astounding increase of 82.56% over the last 24 hours. The Salmon River near Salmon presents a steadier condition, with a flow of 1,260 cfs, only slightly above normal, which may be reassuring for communities and river users along this stretch. The Payette River at Payette reflects a 77.86% of the normal flow, supporting activities like fishing and rafting. With river conditions rapidly changing, those planning to use Idaho's rivers for recreation or other purposes should stay updated on local water levels and flow changes, particularly in spring when snowmelt significantly influences river conditions.

       



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.


       

Winter Storm Warnings

January 2 2026

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