Photograph of custom boogie board for ADCP deploymet, view of bottom.
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Photograph of custom boogie board for ADCP deploymet, view of bottom.
Photograph of custom boogie board for ADCP deploymet, view of bottom.
Photograph of custom boogie board for ADCP deploymet, view of bottom.
Photograph of OceanScience, Inc. rough water trimaran boat for the StreamPro.
Photograph of OceanScience, Inc. rough water trimaran boat for the StreamPro.
A SonTek Argonaut mounting plate is fastened to 2" conduit using a structural pipe wall flange.
A SonTek Argonaut mounting plate is fastened to 2" conduit using a structural pipe wall flange.
Fog Over Glacial Ridge National Wildlife Refuge
Fog Over Glacial Ridge National Wildlife Refuge
Photo of stream in urban environment with green lawn beside it. Photo credit: Alan Cressler USGS
Photo of stream in urban environment with green lawn beside it. Photo credit: Alan Cressler USGS
The AVM-measured velocity used to index mean velocity can be the line velocity from one acoustic path or from multiple acoustic paths.
The AVM-measured velocity used to index mean velocity can be the line velocity from one acoustic path or from multiple acoustic paths.
Protective housing prevents damage to ADVM and allows for adjustment of heading and roll.
Protective housing prevents damage to ADVM and allows for adjustment of heading and roll.
Kentucky mount constructed from Speed Rail. This mount can be used to deploy Rio Grande, RiverPro, RioPro, and RiverSurveyor ADCPs.
Kentucky mount constructed from Speed Rail. This mount can be used to deploy Rio Grande, RiverPro, RioPro, and RiverSurveyor ADCPs.
Old custom made Kentucky-style mount on several different boats from Kentucky and Illinois deploying both Broadband (BB) and Rio Grande ADCPs. A pole can be fixed to the mount for deploying a GPS antenna located on top of the ADCP. The Kentucky-style mount constructed of Speed Rail is recommended for Rio Grande Workhorse, RiverPro, RioPro, and Sontek M9.
Old custom made Kentucky-style mount on several different boats from Kentucky and Illinois deploying both Broadband (BB) and Rio Grande ADCPs. A pole can be fixed to the mount for deploying a GPS antenna located on top of the ADCP. The Kentucky-style mount constructed of Speed Rail is recommended for Rio Grande Workhorse, RiverPro, RioPro, and Sontek M9.
2-speed sailing winch used by the Illinois Field Office to make low-flow measurements on a tagline.
2-speed sailing winch used by the Illinois Field Office to make low-flow measurements on a tagline.
Photograph of tethered boat deployed downstream from a bridge.
Photograph of tethered boat deployed downstream from a bridge.
Q-Boat 1800RP for swift flow.
Q-Boat 1800RP for swift flow.
Young Moose, Glacial Ridge National Wildlife Refuge
Young Moose, Glacial Ridge National Wildlife RefugeYoung moose near Benoit, Minnesota, Glacial Ridge National Wildlife Refuge
Young Moose, Glacial Ridge National Wildlife Refuge
Young Moose, Glacial Ridge National Wildlife RefugeYoung moose near Benoit, Minnesota, Glacial Ridge National Wildlife Refuge
Ephemeral wetlands at Glacial Ridge National Wildlife Refuge
Ephemeral wetlands at Glacial Ridge National Wildlife Refuge
A frontal view of the USGS Water Science Center in Louisville, Kentucky.
A frontal view of the USGS Water Science Center in Louisville, Kentucky.
USGS scientists install a double ring infiltrometer
USGS scientists install a double ring infiltrometerIn this photo, USGS scientists Megan Haserodt (Hydrologist) and Jenelle Wempner (Student Intern) install a double ring infiltrometer along a recreated floodplain of Underwood Creek, a tributary to the Milwaukee River and Lake Michigan in Milwaukee, Wisconsin.
USGS scientists install a double ring infiltrometer
USGS scientists install a double ring infiltrometerIn this photo, USGS scientists Megan Haserodt (Hydrologist) and Jenelle Wempner (Student Intern) install a double ring infiltrometer along a recreated floodplain of Underwood Creek, a tributary to the Milwaukee River and Lake Michigan in Milwaukee, Wisconsin.
USGS employee prepares unmanned aerial vehicle for takeoff
USGS employee prepares unmanned aerial vehicle for takeoffUSGS employee John Fulton prepares an unmanned aerial vehicle for take off. This particular drone referred to as "Q-Cam" measures surface water stream velocity. Combined with a second drone, non-contact discharge measurements can be made.
USGS employee prepares unmanned aerial vehicle for takeoff
USGS employee prepares unmanned aerial vehicle for takeoffUSGS employee John Fulton prepares an unmanned aerial vehicle for take off. This particular drone referred to as "Q-Cam" measures surface water stream velocity. Combined with a second drone, non-contact discharge measurements can be made.
USGS employees point out the newly installed thermal camera
USGS employees point out the newly installed thermal cameraUSGS scientists Adam Baldwin and Chris Gazoorian (USGS New York Water Science Center) point out the newly installed fixed-mount thermal infrared camera installed on the USGS Platte Kill at Dunraven NY streamgage in t
USGS employees point out the newly installed thermal camera
USGS employees point out the newly installed thermal cameraUSGS scientists Adam Baldwin and Chris Gazoorian (USGS New York Water Science Center) point out the newly installed fixed-mount thermal infrared camera installed on the USGS Platte Kill at Dunraven NY streamgage in t
Profilers measure velocities in uniformly-sized cells or bins along the acoustic beams (fig 1). By measuring velocities in a number of bins across a channel or vertically through the water column, these instruments produce horizontal or vertical water velocity profiles, hence the designation "profiler.
Profilers measure velocities in uniformly-sized cells or bins along the acoustic beams (fig 1). By measuring velocities in a number of bins across a channel or vertically through the water column, these instruments produce horizontal or vertical water velocity profiles, hence the designation "profiler.
The AVM measures the average water velocity along the acoustic path (VP, figure 1); then computes the "line velocity," the velocity component parallel with the average downstream flow line.
The AVM measures the average water velocity along the acoustic path (VP, figure 1); then computes the "line velocity," the velocity component parallel with the average downstream flow line.