Training participant holds the rope that is tethered to an acoustic doppler current profiler (ADCP). The ADCP is ferried back and forth the channel while it collects streamflow data.
Images
Check out photos of some of the awesome work USGS scientists and field technicians have done over the years.
![See caption](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/1000000284.jpg?itok=BeTfHxj4)
Training participant holds the rope that is tethered to an acoustic doppler current profiler (ADCP). The ADCP is ferried back and forth the channel while it collects streamflow data.
Measuring streamflow from a human powered cable car takes a lot of skill and quick thinking. A flow meter is lowered into the water using a reel.
Measuring streamflow from a human powered cable car takes a lot of skill and quick thinking. A flow meter is lowered into the water using a reel.
Sometimes climbing up on top of a gage house is necessary to check on the condition of the solar panel and satellite antenna.
Sometimes climbing up on top of a gage house is necessary to check on the condition of the solar panel and satellite antenna.
Esteemed Hydrologic Technician, Katie Baker, measures streamflow with an acoustic doppler current profiler (ADCP). The ADCP tracks the velocity of particles in the water and maps the channel bottom, combine that data with channel width and you can calculate stream flow!
Esteemed Hydrologic Technician, Katie Baker, measures streamflow with an acoustic doppler current profiler (ADCP). The ADCP tracks the velocity of particles in the water and maps the channel bottom, combine that data with channel width and you can calculate stream flow!
One of our incredible hydrologic technicians is in full safety gear, including fall protection and life vest, as she surveys elevation levels. In this photo the white level marker rod has fallen onto the pile of floating logs. It was safely retrieved!
One of our incredible hydrologic technicians is in full safety gear, including fall protection and life vest, as she surveys elevation levels. In this photo the white level marker rod has fallen onto the pile of floating logs. It was safely retrieved!
Hydrologic technicians use electronic tapes to measure groundwater in wells. The tape beeps or lights up when makes contact with water.
Hydrologic technicians use electronic tapes to measure groundwater in wells. The tape beeps or lights up when makes contact with water.
An electronic measuring tape will beep when it hits the surface of the water. This well inspection caught the attention of a neighborhood cat.
An electronic measuring tape will beep when it hits the surface of the water. This well inspection caught the attention of a neighborhood cat.
Grey and black PVC piping housing the water-quality sensors for this stream gage.
Grey and black PVC piping housing the water-quality sensors for this stream gage.
A floating water-quality station that can only be accessed by boat! Sensors hang in the water below the platform. The data is collected and transmits via satellite to the internet.
A floating water-quality station that can only be accessed by boat! Sensors hang in the water below the platform. The data is collected and transmits via satellite to the internet.
![White PVC pipe mounted to a tree along the river bank](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/20230809_153822.jpg?itok=VULglqXM)
A tree mounted white PVC pipe houses water-quality sensors along the South Santiam River.
A tree mounted white PVC pipe houses water-quality sensors along the South Santiam River.
![Leafy trees line opposite bank. Waters on the wide river are green & blue](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/IMG_6810.jpg?itok=GLqGlqGD)
The grey PVC pipe is securely mounted on the river bank to house water-quality instruments.
The grey PVC pipe is securely mounted on the river bank to house water-quality instruments.
A USGS hat sits on a bed of black bear berry vegetation. This photo was taken in Kanuti, Alaska.
A USGS hat sits on a bed of black bear berry vegetation. This photo was taken in Kanuti, Alaska.
Essential gear for measuring streamflow above large rivers. Within this cable car a reel connects to a Price AA flowmeter and sounding weight. Hydrologic technicians reel down the weight until they hit the river bottom, input the total depth into the AquaCalc, then they measure the flow within the water column at various depths to best capture water velocities.
Essential gear for measuring streamflow above large rivers. Within this cable car a reel connects to a Price AA flowmeter and sounding weight. Hydrologic technicians reel down the weight until they hit the river bottom, input the total depth into the AquaCalc, then they measure the flow within the water column at various depths to best capture water velocities.
A high water day at Hood River. Taken while hydrologic technicians out in the field collect streamflow data.
A high water day at Hood River. Taken while hydrologic technicians out in the field collect streamflow data.
Sediment samplers are designed to obtain representative samples across all depths and locations in a river cross-section. This is important because sediment concentrations are not always consistent across the channel. This D-74 sampler weighs 62 pounds and can sample in velocities up to 6.6 feet per second and depths up to 15 feet. It has been in use since 1974.
Sediment samplers are designed to obtain representative samples across all depths and locations in a river cross-section. This is important because sediment concentrations are not always consistent across the channel. This D-74 sampler weighs 62 pounds and can sample in velocities up to 6.6 feet per second and depths up to 15 feet. It has been in use since 1974.
Photo taken during the Green Peter Reservoir drawdown The water is brown due to suspended sediment loads.
Photo taken during the Green Peter Reservoir drawdown The water is brown due to suspended sediment loads.
![Brown water meets clear water](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/FB_IMG_1700597755495.jpg?itok=O7gi6QYW)
A striking contrast between the clear water in the Middle Fork Willamette River and brown water in Fall Creek. The flows from Fall Creek dam during this time had heavy loads of suspended sediment from the reservoir drawdown.
A striking contrast between the clear water in the Middle Fork Willamette River and brown water in Fall Creek. The flows from Fall Creek dam during this time had heavy loads of suspended sediment from the reservoir drawdown.
Researcher collecting depth, velocity, water surface elevation, and 360 degree imagery on the North Santiam River.
Researcher collecting depth, velocity, water surface elevation, and 360 degree imagery on the North Santiam River.
River bed-sediment size and distribution is critical for fish spawning habitat. The kayaking scientist in this photo is towing an advanced acoustic instrument that measures river velocity and depth. In addition, a camera captures photos that can be used to create digital elevation models and eventually maps of river bed-sediment size.
River bed-sediment size and distribution is critical for fish spawning habitat. The kayaking scientist in this photo is towing an advanced acoustic instrument that measures river velocity and depth. In addition, a camera captures photos that can be used to create digital elevation models and eventually maps of river bed-sediment size.
Researchers prep equipment before a river mapping survey on the Niagara section of the North Santiam River.
Researchers prep equipment before a river mapping survey on the Niagara section of the North Santiam River.