Kevin A Oberg (Former Employee)
Science and Products
Filter Total Items: 65
Hydroacoustic Current Meters for the Measurement of Discharge in Shallow Rivers and Streams Hydroacoustic Current Meters for the Measurement of Discharge in Shallow Rivers and Streams
The U.S. Geological Survey (USGS) is evaluating the use of hydroacoustic current meters for making discharge measurements in shallow rivers and streams. The USGS historically has made discharge measurements in shallow rivers using mechanical, impellor-type current meters attached to a wading rod. The evaluation project has focused on three categories of hydroacoustic meters: an acoustic...
Authors
S. E. Morlock, G. T. Fisher
Looking to the Future: Non-contact Methods for Measuring Streamflow Looking to the Future: Non-contact Methods for Measuring Streamflow
We have conducted a series of proof-of-concept experiments to demonstrate whether it is possible to make completely non-contact open-channel discharge measurements. After an extensive evaluation of potential technologies, we concluded a combination of high-frequency (microwave) radar (for measuring surface velocity) and low-frequency radar (ground-penetrating radar) for measuring channel...
Authors
J. E. Costa, R. T. Cheng, F.P. Haeni, N.B. Melcher, K.R. Spicer, J. Plant, W.C. Keller, K. Hayes
Experimental Acoustic Velocity Measurements in a Tidally Affected Stream Experimental Acoustic Velocity Measurements in a Tidally Affected Stream
The U.S. Geological Survey (USGS) constructed a continuous steamgaging station on the tidally affected Escatawpa River at Interstate 10 near Orange Grove, Mississippi, in August 2001. The gage collects water quantity parameters of stage and stream velocity, and water quality parameters of water temperature, specific conductance, and salinity. Data are transmitted to the local USGS office...
Authors
J.B. Storm
Ice-affected streamflow records using tracer-dilution discharge methods Ice-affected streamflow records using tracer-dilution discharge methods
Accurate ice-affected streamflow records are difficult to obtain for several reasons. Problems measuring stage, variable backwater conditions, access limitations in wintertime, and problems measuring flowing water under ice cover all contribute to make ice-affected streamflow records less accurate than open-channel streamflow records. The inaccuracy of ice-affected streamflow records is
Authors
J.P. Capesius, J.R. Sullivan, C.A. Williams, G. B. O’Neill
Discharge Measurements in Shallow Urban Streams Using a Hydroacoustic Current Meter Discharge Measurements in Shallow Urban Streams Using a Hydroacoustic Current Meter
Hydroacoustic current-meter measurements were evaluated in small urban streams under a range of stages, velocities, and channel-bottom materials. Because flow in urban streams is often shallow, conventional mechanical current-meter measurements are difficult or impossible to make. The rotating-cup Price pygmy meter that is widely used by the U.S. Geological Survey and other agencies...
Authors
G. T. Fisher, S. E. Morlock
Measurement of the bed material of gravel-bed rivers Measurement of the bed material of gravel-bed rivers
The measurement of the physical properties of a gravel-bed river is important in the calculation of sediment transport and physical habitat values for aquatic animals. These properties are not always easy to measure. One recent report on flushing of fines from the Klamath River did not contain information on one location because the grain size distribution of the armour could not be...
Authors
R.T. Milhous
Science and Products
Filter Total Items: 65
Hydroacoustic Current Meters for the Measurement of Discharge in Shallow Rivers and Streams Hydroacoustic Current Meters for the Measurement of Discharge in Shallow Rivers and Streams
The U.S. Geological Survey (USGS) is evaluating the use of hydroacoustic current meters for making discharge measurements in shallow rivers and streams. The USGS historically has made discharge measurements in shallow rivers using mechanical, impellor-type current meters attached to a wading rod. The evaluation project has focused on three categories of hydroacoustic meters: an acoustic...
Authors
S. E. Morlock, G. T. Fisher
Looking to the Future: Non-contact Methods for Measuring Streamflow Looking to the Future: Non-contact Methods for Measuring Streamflow
We have conducted a series of proof-of-concept experiments to demonstrate whether it is possible to make completely non-contact open-channel discharge measurements. After an extensive evaluation of potential technologies, we concluded a combination of high-frequency (microwave) radar (for measuring surface velocity) and low-frequency radar (ground-penetrating radar) for measuring channel...
Authors
J. E. Costa, R. T. Cheng, F.P. Haeni, N.B. Melcher, K.R. Spicer, J. Plant, W.C. Keller, K. Hayes
Experimental Acoustic Velocity Measurements in a Tidally Affected Stream Experimental Acoustic Velocity Measurements in a Tidally Affected Stream
The U.S. Geological Survey (USGS) constructed a continuous steamgaging station on the tidally affected Escatawpa River at Interstate 10 near Orange Grove, Mississippi, in August 2001. The gage collects water quantity parameters of stage and stream velocity, and water quality parameters of water temperature, specific conductance, and salinity. Data are transmitted to the local USGS office...
Authors
J.B. Storm
Ice-affected streamflow records using tracer-dilution discharge methods Ice-affected streamflow records using tracer-dilution discharge methods
Accurate ice-affected streamflow records are difficult to obtain for several reasons. Problems measuring stage, variable backwater conditions, access limitations in wintertime, and problems measuring flowing water under ice cover all contribute to make ice-affected streamflow records less accurate than open-channel streamflow records. The inaccuracy of ice-affected streamflow records is
Authors
J.P. Capesius, J.R. Sullivan, C.A. Williams, G. B. O’Neill
Discharge Measurements in Shallow Urban Streams Using a Hydroacoustic Current Meter Discharge Measurements in Shallow Urban Streams Using a Hydroacoustic Current Meter
Hydroacoustic current-meter measurements were evaluated in small urban streams under a range of stages, velocities, and channel-bottom materials. Because flow in urban streams is often shallow, conventional mechanical current-meter measurements are difficult or impossible to make. The rotating-cup Price pygmy meter that is widely used by the U.S. Geological Survey and other agencies...
Authors
G. T. Fisher, S. E. Morlock
Measurement of the bed material of gravel-bed rivers Measurement of the bed material of gravel-bed rivers
The measurement of the physical properties of a gravel-bed river is important in the calculation of sediment transport and physical habitat values for aquatic animals. These properties are not always easy to measure. One recent report on flushing of fines from the Klamath River did not contain information on one location because the grain size distribution of the armour could not be...
Authors
R.T. Milhous
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government