USGS Nebraska Water Science Center hydrologic technician, Nathan Shultz, collecting depth and velocity data at the USGS streamgaging station 06453600 Ponca Creek at Verdel, Nebraska during an ice jam on February 15, 2017.
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USGS Nebraska Water Science Center hydrologic technician, Nathan Shultz, collecting depth and velocity data at the USGS streamgaging station 06453600 Ponca Creek at Verdel, Nebraska during an ice jam on February 15, 2017.
Hydrologic Technician, James Albrecht, from the North Platte Field Office making a measurement of discharge under ice using a Flowtracker acoustic velocity meter on a top-setting wading rod. The string going across the picture is a tagline, used for measuring distance across the channel so that he can note the location of the ice hole he is working in. T
Hydrologic Technician, James Albrecht, from the North Platte Field Office making a measurement of discharge under ice using a Flowtracker acoustic velocity meter on a top-setting wading rod. The string going across the picture is a tagline, used for measuring distance across the channel so that he can note the location of the ice hole he is working in. T
Agricultural tile drain emptying into waterway.
Agricultural tile drain emptying into waterway.
Tile drain in eastern Nebraska equipped with monitoring instruments.
Tile drain in eastern Nebraska equipped with monitoring instruments.
This view is looking south to the Dismal River from the U.S. Highway 83 scenic overlook south of Thedford, Nebraska.
This view is looking south to the Dismal River from the U.S. Highway 83 scenic overlook south of Thedford, Nebraska.
During the summer of 2013, the Nebraska Sandhills exhibited a unusually significant sunflower emergence probably triggered by environmental conditions from the preceeding 2012 drought. Also, the Eastern Red Cedar is a particularly agressive invasive species which has become well established in Nebraska.
During the summer of 2013, the Nebraska Sandhills exhibited a unusually significant sunflower emergence probably triggered by environmental conditions from the preceeding 2012 drought. Also, the Eastern Red Cedar is a particularly agressive invasive species which has become well established in Nebraska.
The Dismal River valley is far from "dismal." Set in the Nebraska Sandhills, this idyllic river is relatively unaffected by humans and a popular recreational river in the state. The invasive species Eastern Red Cedar has become well established in Nebraska.
The Dismal River valley is far from "dismal." Set in the Nebraska Sandhills, this idyllic river is relatively unaffected by humans and a popular recreational river in the state. The invasive species Eastern Red Cedar has become well established in Nebraska.
This is a panoramic view of the Dismal River and the Nebraska Sandhills.
This is a panoramic view of the Dismal River and the Nebraska Sandhills.
Platte River from the observation tower near South Bend, Nebraska.
Platte River from the observation tower near South Bend, Nebraska.
USGS Nebraska Water Science Center hydrologist, Greg Steele, collecting groundwater level measurements at night during an aquifer test.
USGS Nebraska Water Science Center hydrologist, Greg Steele, collecting groundwater level measurements at night during an aquifer test.
USGS Nebraska Water Science Center Elkhorn-Loup Model project chief, Steve Peterson, making a stream discharge measurement. The project collected hundreds of discharge measurements in 2006 to determine base flow in the study area.
USGS Nebraska Water Science Center Elkhorn-Loup Model project chief, Steve Peterson, making a stream discharge measurement. The project collected hundreds of discharge measurements in 2006 to determine base flow in the study area.
Platte River near Alda, Nebraska at sunset, Nov. 6, 2006.
Platte River near Alda, Nebraska at sunset, Nov. 6, 2006.
Wetlands in the Nebraska Sandhills typically are at the groundwater and surface water interface. You are essentially seeing the groundwater level in the area.
Wetlands in the Nebraska Sandhills typically are at the groundwater and surface water interface. You are essentially seeing the groundwater level in the area.