How to Measure the Water Current of the Yellowstone River

Explore how to measure the Yellowstone River's current using ADCP, its working principle, and equipment selection for accurate hydrographic analysis.

1. Where is the Yellowstone River?

The Yellowstone River is a phenomenal and iconic water body in the United States. It originates in the Absaroka Range of Wyoming, close to Yellowstone National Park. Further, it meanders through a varied and dramatic landscape that comprises all sorts of park geothermal features, such as geysers, hot springs, and mud pots.

As it leaves the park, it continues on through Montana, carving through canyons like the Yellowstone River Canyon with stunning rock formations. It flows across plains and valleys until it passes by numerous small towns and ranches, relying on the river for water supply and irrigation.

The Yellowstone River is an important part of the local ecosystem and at the same time an important draw for tourism. It offers opportunities for activities like fishing, rafting, and boating. Various trout species abound in its waters and attract anglers from far and wide. The riverbanks are habitats for numerous wildlife species, from elk and deer coming to drink to bald eagles soaring above in search of fish. The floodplains and wetlands associated with the river contribute much to the ecological balance, being nesting and feeding places for a number of bird species and other animals.

2. What is the flow rate in the Yellowstone River like?

The flow rate in the Yellowstone River has large seasonal variations. During the spring, when snow melts originating from the surrounding mountains, including the Absaroka Range and other high elevations of its catchment area, there is a large rise in the flow of the river. As it melts, the snow sends a volume of water downstream, with relatively high flow.

While it gradually decreases due to the snowmelt influence which is wearing off, and also the patterns of precipitation change during the summer and fall seasons, it still maintains a base flow that is vital for the mere existence of aquatic life and to support the different water-dependent activities for irrigation of local agriculture. In winter, this can be even smaller, and, in severe cold snaps, portions of the river can freeze over entirely. Consequently, the average flow rate may range from a few hundred cubic meters per second during the low-flow periods to several thousand cubic meters per second during the peak of the spring snowmelt.

3. How to measure water current of the Yellowstone River?

Velocity Meter Method

The traditional approach utilizes mechanical or electronic velocity meters. The equipment is stationed at various points within the flow of the river to directly measure the speed of the water in that particular area. But to have an overall understanding of the current of the water, many measurements are taken at various depths and over different areas of the river. With the variable nature of the conditions along this very long Yellowstone River, this can be quite labor-intensive and time-consuming.

ADCP Method

The ADCP method represents a more advanced and convenient means of measuring water currents. It uses sound waves as a medium to detect the motion of water particles. The instrument emits acoustic signals and measures the Doppler shift of the reflected signals back to estimate the water velocity at several depths simultaneously. This gives a very accurate profile of the water current and thereby furnishes more actual flow conditions down the river. The ADCP can be mounted on boats or bridges or even deployed on buoys for continuous monitoring.

Buoy Method

In the buoy method, buoys are put into the river, which are fitted with sensors to measure the movement of water around the buoys. These buoys float on the surface and may give some sort of signal about the surface current, but they may fail to capture the full complexity of the water current as accurately as in the above methods, especially while knowing the variability of the velocity at different depths.

Of all those methods, the ADCP current profiler is a more advanced and proficient way of measuring the water current of the Yellowstone River.

4. How do ADCPs using the principle of Doppler work?

The principle involved in ADCPs is the Doppler principle. When an ADCP flow meter sends out its acoustic signal into the water, the sound waves travel through the water and interact with moving water particles. Because the water particles are moving, the frequency of the reflected sound waves changes because of the Doppler effect.

If the water particles are moving towards the ADCP meter, then the reflected wave frequency is higher than the emitted frequency. In turn, when the water particles are moving away from the ADCP profiler, the frequency of the reflected wave becomes lower. The precise measurement of this change in frequency allows the ADCP to compute the velocity of the water particles at different depths.

Then, the ADCP meter combines these individual velocity measurements at differing depths to provide a complete profile of the water current. In this way, it is possible to obtain a thorough knowledge of the flow of water, not only at the surface but throughout the vertical section of the river.

5. What is necessary for high-quality measurement of currents of the Yellowstone River?

For high-quality measurement of the currents of the Yellowstone River, the equipment needs to have certain features.

The material reliability of the equipment should be high. Since the equipment has to bear the harsh river environmental conditions that include exposure to water and sediment, as well as variable temperatures, it should be robust. Similarly, due to the variable flow of the Yellowstone River and debris during high-flow seasons, it needs strong equipment.

Besides, the small size and lightweight with low power consumption are also wanted. A compact and light gadget is simpler to manipulate and deploy either on a boat or attached to a buoy. Low power consumption ensures that equipment could work for extended periods without any need for frequent battery replacements or access to a continuous power source.

Cost - effectiveness is an important factor. A lower - cost option enables more widespread use of the measurement equipment, allowing for more comprehensive monitoring of the river.

When it comes to the casing of the ADCP flow meter, titanium alloy is an excellent choice. The resistance to corrosion is very high in the titanium alloy, which is vital in this case, when water bodies are dealt with, such as the Yellowstone River, where equipment will always be in contact with water and other substances that may be corrosive. It is also strong, durable, and resistant to impacts and to changes in pressure that may occur during deployment and operation. The density of titanium alloy is relatively low, so it contributes to the goal of keeping the equipment lightweight.

6. How to Choose the right equipment for current measurement?

In choosing the right equipment to measure the current of the Yellowstone River, several factors should be considered.

Based on the Purpose of Use

To measure the horizontal cross - section, one would want an ADCP current profiler in a horizontal position, therefore called a horizontal ADCP. HADCPs are designed to deliver high-accuracy readings of water flow in the horizontal plane to help in understanding the overall movement of water across any given section of the river.

In case the target is to measure the vertical sectioning of the current in the river, one should opt for a vertical ADCP current meter. Vertical ADCPs can measure the water velocities at each depth with high resolution, providing a detailed profile of how the water flows vertically in the river.

Frequency-Based

The exact choice of frequency depends on the depth of the water in the Yellowstone River. For most water depths that are up to 70 meters, a 600 kHz ADCP should be fairly adequate. This frequency provides good resolution and accuracy for measuring the water current in the relatively shallow waters.

In the case of deeper waters, such as those exceeding 70 meters up to about 110 meters, there is a 300 kHz ADCP. A low frequency of 300 kHz can still manage to go deeper into the water and give good measurements of the water current.

There are renowned ADCP brands: Teledyne RDI, Nortek, and Sontek. However, for those seeking a cost - effective option with excellent quality, the China Sonar PandaADCP is worth considering. It is made of all - titanium alloy material, ensuring durability and reliability. With its remarkable cost - performance ratio, it provides a great alternative for measuring the water current of the Yellowstone River. You can find more information about it on its official website: https://china-sonar.com/.

Here is a table with some well known ADCP instrument brands and models.

Brand model
Teledyne RDI Ocean Surveyor ADCP, Pinnacle ADCP, Sentinel V ADCP, Workhorse II Monitor ADCP, Workhorse II Sentinel ADCP, Workhorse II Mariner ADCP, Workhorse Long Ranger ADCP, RiverPro ADCP, RiverRay ADCP, StreamPro ADCP, ChannelMaster ADCP, etc.
NORTEK Eco, Signature VM Ocean, Signature, AWAC, Aquadopp Profiler, etc.
SonTek  SonTek-RS5, SonTek-M9, SonTek-SL, SonTek-IQ, etc.
China Sonar PandaADCP-DR-600K, PandaADCP-SC-300K, PandaADCP-DR-300K,PandaADCP-SC-600K, PandaADCP-DR-75K-PHASED, etc.
Jack Law October 31, 2024
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