Last Updated: January 2, 2026
Washington State's streamflow conditions exhibit varied trends across different river systems, with some waterways experiencing below-normal flows indicative of potential drought conditions, while others are maintaining healthier volumes. Notably, the Spokane River at Spokane presents an elevated streamflow at 181.28% of normal, raising concerns for possible flooding in the surrounding areas, including the city of Spokane. Contrastingly, Hangman Creek at Spokane shows a significant drop in streamflow levels, currently at -58.5% below normal, which could signal flow drought conditions. The Columbia River at the International Boundary reports a streamflow of 93,100 cfs with a slight 0.11% increase in the last 24 hours, but remains low at 2.26% of the usual flow, which could affect large watersheds and potentially impact cities along its course. Additionally, the Methow River near Pateros exhibits a high streamflow change of 159.43% of normal, which could be a concern for recreational activities such as whitewater trails in the area.
Streamflows in major rivers such as the Pend Oreille River below Box Canyon and the Little Spokane River are also notable, with the former flowing at 71.64% of its normal rate with a current streamflow of 29,200 cfs and the latter showing significantly reduced streamflow rates, potentially impacting the river ecosystem and nearby communities. For water enthusiasts, the Wenatchee River at Monitor presents an 88.1% of normal flow that could affect water-based recreation. It is critical for river and whitewater enthusiasts to stay informed about these variable conditions, as they may affect accessibility, safety, and ecological health. Local authorities and recreationalists should closely monitor these waterways for any rapid changes that could indicate either escalation towards flooding or progression towards drought conditions, depending on the region within Washington State.
Washington state is characterized by a diverse hydrology that is heavily influenced by its climate and geological features. The state's major surface flows are the Columbia River, Snake River, Yakima River, and Spokane River. These rivers are fed by numerous tributaries and are regulated by large reservoirs such as the Grand Coulee Dam and the Bonneville Dam. The state's mountainous terrain and heavy snowfall create significant watershed systems that contribute to river flow, with the snowpack in the Cascade Range being a primary contributor. Climate patterns such as El Niño and La Niña can impact precipitation rates and snowpack levels, leading to drought or flooding events. Overall, the hydrology of Washington is a complex and dynamic system that is heavily influenced by both natural and human factors.
| River Run | Status | Streamflow (CFS) | Air Temp (F) |
|---|---|---|---|
|
Douglas Fir Campground to Mt. Baker Highway
Class II+ to III |
RUNNABLE | 390 | 48 |
|
Rock Island Campground to Ida Creek
Class II+ to III |
36.25 | ||
|
Snoqualmie Falls to Plum's Landing
Class II+ to III- |
RUNNABLE | 398 | 52 |