Paul Kinzel
Paul Kinzel is a Hydrologist with the USGS Water Resources Mission Area.
Education
M.S. in Civil Engineering, University of Colorado, Boulder, May 1998
B.S. in Environmental Science, State University of New York, Plattsburgh, May 1995
Science and Products
Filter Total Items: 39
No Result Found
Filter Total Items: 55
Geomorphic Data Collected Within Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2004
No abstract available.
Authors
Paul J. Kinzel, Randolph S. Parker, Jonathan M. Nelson, Aaron R. Burman, Ashley K. Heckman
Assessing sandhill crane roosting habitatalong the Platte River, Nebraska
Each spring approximately 500,000 sandhill cranes and some endangered whooping cranes use the Central Platte River Valley in Nebraska as a staging habitat during their migration north to breeding and nesting grounds in Canada, Alaska, and the Siberian Arctic. Over the last century changes in the flow of the river have altered the river channels and the distribution of roost sites. USGS researchers
Authors
P.J. Kinzel, J. M. Nelson, R. S. Parker
Geomorphic Data Collected Within and Adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2003
No abstract available.
Authors
Paul J. Kinzel, Randolph S. Parker, Jonathan M. Nelson, Aaron R. Burman, Ashley K. Heckman
Geomorphic data collected within and adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2001
River-channel topographic surveys were conducted and bed-material samples were collected along transects across the Platte River during water year 2001 (October 1, 2000 to September 30, 2001). A total of 57 transect lines or cross sections were established within three study reaches located along the middle channel of the Platte River in a 2,650-acre parcel of land owned by the Nebraska Public Pow
Authors
Paul Kinzel, Randolph Parker, Johnathan Nelson, R. Burman, Aashley Heckman
Geomorphic data collected within and adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2002
River-channel topographic surveys were conducted and bed-material samples were collected along transects across the Platte River during water year 2002 (October 1, 2001 to September 30, 2002). A total of 57 transect lines or cross sections were established within three study reaches located along the middle channel of the Platte River in a 2,650-acre parcel of land owned by the Nebraska Public Pow
Authors
Paul Kinzel, Randolph Parker, Jonathan Nelson, Steven Gyetvai, Aaron Burman, Ashley Heckman
Colorado River sediment transport: 2. Systematic bed‐elevation and grain‐size effects of sand supply limitation
The Colorado River in Marble and Grand Canyons displays evidence of annual supply limitation with respect to sand both prior to [Topping et al, this issue] and after the closure of Glen Canyon Dam in 1963. Systematic changes in bed elevation and systematic coupled changes in suspended‐sand concentration and grain size result from this supply limitation. During floods, sand supply limitation either
Authors
David J. Topping, David M. Rubin, Jonathan M. Nelson, Paul J. Kinzel, Ingrid C. Corson
Linkage between grain-size evolution and sediment depletion during Colorado River floods
No abstract available.
Authors
David J. Topping, David M. Rubin, Jonathan M. Nelson, Paul J. Kinzel, James P. Bennett
Science and Products
Filter Total Items: 39
No Result Found
Filter Total Items: 55
Geomorphic Data Collected Within Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2004
No abstract available.
Authors
Paul J. Kinzel, Randolph S. Parker, Jonathan M. Nelson, Aaron R. Burman, Ashley K. Heckman
Assessing sandhill crane roosting habitatalong the Platte River, Nebraska
Each spring approximately 500,000 sandhill cranes and some endangered whooping cranes use the Central Platte River Valley in Nebraska as a staging habitat during their migration north to breeding and nesting grounds in Canada, Alaska, and the Siberian Arctic. Over the last century changes in the flow of the river have altered the river channels and the distribution of roost sites. USGS researchers
Authors
P.J. Kinzel, J. M. Nelson, R. S. Parker
Geomorphic Data Collected Within and Adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2003
No abstract available.
Authors
Paul J. Kinzel, Randolph S. Parker, Jonathan M. Nelson, Aaron R. Burman, Ashley K. Heckman
Geomorphic data collected within and adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2001
River-channel topographic surveys were conducted and bed-material samples were collected along transects across the Platte River during water year 2001 (October 1, 2000 to September 30, 2001). A total of 57 transect lines or cross sections were established within three study reaches located along the middle channel of the Platte River in a 2,650-acre parcel of land owned by the Nebraska Public Pow
Authors
Paul Kinzel, Randolph Parker, Johnathan Nelson, R. Burman, Aashley Heckman
Geomorphic data collected within and adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2002
River-channel topographic surveys were conducted and bed-material samples were collected along transects across the Platte River during water year 2002 (October 1, 2001 to September 30, 2002). A total of 57 transect lines or cross sections were established within three study reaches located along the middle channel of the Platte River in a 2,650-acre parcel of land owned by the Nebraska Public Pow
Authors
Paul Kinzel, Randolph Parker, Jonathan Nelson, Steven Gyetvai, Aaron Burman, Ashley Heckman
Colorado River sediment transport: 2. Systematic bed‐elevation and grain‐size effects of sand supply limitation
The Colorado River in Marble and Grand Canyons displays evidence of annual supply limitation with respect to sand both prior to [Topping et al, this issue] and after the closure of Glen Canyon Dam in 1963. Systematic changes in bed elevation and systematic coupled changes in suspended‐sand concentration and grain size result from this supply limitation. During floods, sand supply limitation either
Authors
David J. Topping, David M. Rubin, Jonathan M. Nelson, Paul J. Kinzel, Ingrid C. Corson
Linkage between grain-size evolution and sediment depletion during Colorado River floods
No abstract available.
Authors
David J. Topping, David M. Rubin, Jonathan M. Nelson, Paul J. Kinzel, James P. Bennett