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Idaho’s Waterways in Motion: Current River and Stream Flows

Compare the data of seven Idaho river and stream flows, and learn how and why the flow rate on a river is measured.

Idaho is known for its vast network of rivers, which provide a variety of recreational opportunities, including fishing, kayaking, and rafting. In this article post, we will take a closer look at the flow rates of some of Idaho’s biggest rivers.

idaho river flows are measured near the city of Priest River
A beautiful sunrise in the pristine wilderness around the Priest River in Idaho. Shot on 35mm film.

Before we dive into the details, let’s first define what we mean by “flow rate.” The flow rate of a river is simply the volume of water that passes a specific point in the river over a given amount of time, usually measured in cubic feet per second (cfs). This measurement can be affected by a variety of factors, including rainfall, snowmelt, and dam releases.

The water that is flowing through a river at a particular moment and location is called its discharge, or flow. This is usually measured in terms of the amount of water that passes through a given point in a specific unit of time, commonly expressed as cubic feet per second or cubic meters per second. In other words, it’s just a way of quantifying how much water is moving through a river at a particular point in time.

Snake River Flow

The Snake River is the largest river in Idaho, stretching over 1,078 miles and flowing through the southern part of the state. The river begins in Wyoming and travels through Idaho, Washington, and Oregon before emptying into the Columbia River. The Snake River is known for its rugged beauty, excellent fishing, and a variety of recreational opportunities, including rafting, kayaking, and jet boating.

The Snake River has an average discharge of 7,900 cubic feet per second (cfs) and a drainage area of 108,000 square miles. Here’s a table showing the average monthly flows for the Snake River in Idaho.

MonthAverage Flow (cfs)
Jan7,020
Feb8,560
Mar14,100
Apr20,100
May22,500
Jun24,600
Jul24,300
Aug20,700
Sep14,800
Oct10,000
Nov8,190
Dec6,720

Salmon River Flow

The Salmon River is a tributary of the Snake River, stretching over 425 miles and flowing through central Idaho. The river is known for its wild and scenic beauty, excellent fishing, and world-class whitewater rafting. The Salmon River has an average discharge of 4,200 cfs and a drainage area of 14,000 square miles.

Here’s a table showing the average monthly flows for the Salmon River in Idaho.

MonthAverage Flow (cfs)
Jan1,490
Feb1,710
Mar3,090
Apr5,290
May7,280
Jun8,680
Jul9,020
Aug7,790
Sep5,590
Oct3,020
Nov2,020
Dec1,560

Payette River Flow

The Payette River is a 82-mile long river flowing through central Idaho. The river is a popular destination for white water rafting, kayaking, and fishing. The Payette River has an average discharge of 1,400 cfs and a drainage area of 3,240 square miles.

Here’s a table showing the average monthly flows for the Payette River in Idaho.

MonthAverage Flow (cfs)
Jan853
Feb963
Mar1,460
Apr2,330
May3,030
Jun2,510
Jul1,560
Aug947
Sep678
Oct554
Nov559
Dec761

Boise River Flow

The Boise River is a 102-mile long river flowing through southwest Idaho. It is a tributary of the Snake River. The river is a popular destination for recreational activities, including kayaking, fishing, and swimming. The Boise River has an average discharge of 1,300 cfs and a drainage area of 4,100 square miles.

Here’s a table showing the average monthly flows for the Boise River in Idaho.

MonthAverage Flow (cfs)
Jan750
Feb850
Mar1,320
Apr2,320
May2,820
Jun1,620
Jul970
Aug770
Sep540
Oct480
Nov620
Dec740

Priest River Flow

The Priest River is a 68-mile long river in Bonner County that dumps into the Pend Oreille River leading into eastern Washington. The river is a popular destination for fishing, kayaking, and swimming. The Priest River has an average discharge of 780 cfs and a drainage area of 888 square miles.

Here’s a table showing the average monthly flows for the Priest River in Idaho.

MonthAverage Flow (cfs)
Jan564
Feb506
Mar804
Apr1,160
May1,570
Jun1,620
Jul1,070
Aug599
Sep498
Oct535
Nov573
Dec578

Coeur d’Alene River Flow

The Coeur d’Alene River is a 37-mile long river flowing through northern Idaho. The river is a popular destination for fishing, kayaking, and rafting. The Coeur d’Alene River has an average discharge of 700 cfs and a drainage area of 1,300 square miles.

Here’s a table showing the average monthly flows for the Coeur d’Alene River in Idaho.

MonthAverage Flow (cfs)
Jan368
Feb419
Mar728
Apr1,720
May2,870
Jun2,140
Jul1,140
Aug712
Sep538
Oct502
Nov429
Dec356

Clearwater River Flow

The Clearwater River is a 75-mile long river flowing through north-central Idaho. The river is a popular destination for recreational activities, including fishing, boating, and camping. The Clearwater River has an average discharge of 6,800 cfs and a drainage area of 9,650 square miles.

Here’s a table showing the average monthly flows for the Clearwater River in Idaho.

MonthAverage Flow (cfs)
Jan2,880
Feb3,520
Mar7,320
Apr17,300
May25,200
Jun21,700
Jul13,600
Aug9,030
Sep6,550
Oct5,410
Nov4,630
Dec3,440

Why is river flow rate measured?

Understanding the flow rate of a river is crucial for many reasons. It can help us predict and prepare for floods, droughts, and other water-related hazards. It is also important for managing and allocating water resources for human use, agriculture, and industry.

Geologists use river flow rate data to study the hydrologic cycle, which is the process by which water moves through the earth’s atmosphere, land, and oceans. This information can help geologists understand how water shapes the landscape over time and how it interacts with other natural processes like erosion, weathering, and sediment transport.

It’s an important flow rate data is an important tool for scientists, engineers, and policymakers who are working to manage and protect our planet’s water resources. By studying and monitoring river flows, we can better understand and manage this precious resource for the benefit of all.

Who measures the flow rate of a river?

In Idaho, the US Geological Survey (USGS) is primarily responsible for collecting and maintaining river flow rate data. The USGS has a network of gauging stations throughout the state that continuously monitor the flow of rivers and streams. This data is then made publicly available on the USGS website for anyone to access and use.

In addition to the USGS, other agencies and organizations in Idaho may also collect and use river flow rate data for various purposes, such as managing water resources or monitoring environmental conditions.

However, the USGS is the primary source for this data in Idaho and is considered the most reliable and comprehensive source of information on river flows in the state.

How does the USGS measure the Idaho river flows?

One of the most common methods used to measure flow rate is to use a stream gauges which continuously monitor water levels in a river or stream.

Stream gauges work by measuring the height of the water surface at a particular point in the river and then using that measurement, along with other factors such as the width and slope of the river, to calculate the flow rate. Some gauges also use acoustic sensors or other technologies to measure the velocity of the water as it flows past the gauge.

In addition to stream gauges, the USGS uses tracer studies and aerial photography.

Tracer studies involve adding a small amount of a harmless chemical to the water and then tracking how it moves downstream, which can help determine the speed and direction of the water flow.

Aerial photography can also be used to estimate flow rate by analyzing the patterns of water movement and other characteristics visible from above.

Frequently
Asked
Questions

What else did you need to know that we didn’t cover? Send us an email and we’ll help you find the answer.

When it rains, the water can either soak into the ground or run off the surface, and that runoff travels downhill, gathering in streams and lakes, and eventually making its way to the ocean. This happens because of gravity – water naturally moves from higher elevations to lower elevations. That’s basically how rivers are formed!


The main distinction between rivers and streams is primarily based on the size and flow velocity of the water. Rivers are typically more extensive and carry a higher volume of water compared to streams. Specifically, rivers are permanent bodies of water that flow from one region to another, usually through a defined channel or bed. This is in contrast to streams, which are generally smaller and may have an intermittent flow. So, in essence, rivers and streams differ mainly in terms of their size, permanence, and the volume of water they carry.

A river’s speed can range from almost zero meters per second to about 3.1 meters per second, which is equivalent to roughly 7 miles per hour. Several factors can influence the velocity of a river, including the steepness of its slope, the roughness of the channel, and the presence of tides. Typically, rivers flow downhill, from higher to lower elevations, and the steepness of this slope is known as the gradient. Therefore, the gradient of a river plays a crucial role in determining its speed. Essentially, a river’s speed is influenced by several complex and interconnected factors that contribute to its flow rate.

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