Donald O Rosenberry (Former Employee)
Science and Products
Filter Total Items: 132
Hydrology of prairie pothole wetlands during drought and deluge: A 17-year study of the Cottonwood Lake wetland complex in North Dakota in the perspective of longer term measured and proxy hydrological records
From 1988 to 1992 the north-central plains of North America had a drought that was followed by a wet period that continues to the present (1997). Data on the hydrology of the Cottonwood Lake area (CWLA) collected for nearly 10 years before, and during, the recent dry and wet periods indicate that some prairie pothole wetlands served only a recharge function under all climate conditions. Transpirat
Authors
T. C. Winter, D. O. Rosenberry
Hydrologic functions of prairie wetlands
Wetlands in the prairie known as potholes or sloughs represent an ever-changing mosaic of surface waters interacting with the atmosphere, groundwater, and each other in a variety of ways. Studies of groups of adjacent wetlands in different parts of the glaciated North American prairie have enabled some connections to be made between hydrologic processes, biological communities, and use of these we
Authors
J. W. LaBaugh, T. C. Winter, D. O. Rosenberry
Evaporation from a small prairie wetland in the Cottonwood Lake Area, North Dakota - An energy-budget study
Evaporation from Wetland Pl in the Cottonwood Lake area of North Dakota, USA was determined by the energy-budget method for 1982-85 and 1987. Evaporation rates were as high as 0.672 cm day-1. Incoming solar radiation, incoming atmospheric radiation, and long-wave radiation emitted from the water body are the largest energy fluxes to and from the wetland. Because of the small heat storage of the wa
Authors
R.S. Parkhurst, T. C. Winter, D. O. Rosenberry, A.M. Sturrock
Watershed-scale research from many perspectives : the Interdisciplinary Research Initiative at the Shingobee River headwaters area, Minnesota
No abstract available.
Authors
D. O. Rosenberry
Hydrological and chemical estimates of the water balance of a closed-basin lake in north central Minnesota
Chemical mass balances for sodium, magnesium, chloride, dissolved organic carbon, and oxygen 18 were used to estimate groundwater seepage to and from Williams Lake, Minnesota, over a 15-month period, from April 1991 through June 1992. Groundwater seepage to the lake and seepage from the lake to groundwater were determined independently using a flow net approach using data from water table wells in
Authors
James W. LaBaugh, Thomas C. Winter, Donald O. Rosenberry, Paul F. Schuster, Michael M. Reddy, George R. Aiken
Dynamics of water-table fluctuations in an upland between two prairie-pothole wetlands in North Dakota
Data from a string of instrumented wells located on an upland of 55 m width between two wetlands in central North Dakota, USA, indicated frequent changes in water-table configuration following wet and dry periods during 5 years of investigation. A seasonal wetland is situated about 1.5 m higher than a nearby semipermanent wetland, suggesting an average ground water-table gradient of 0.02. However,
Authors
Donald O. Rosenberry, Thomas C. Winter
Hydrological and biogeochemical research in the Shingobee River headwaters area, north-central Minnesota
No abstract available.
Authors
Thomas C. Winter
Changes in atmospheric circulation patterns affect midcontinent wetlands sensitive to climate
Twenty-seven years of data from midcontinent wetlands indicate that the response of these wetlands to extremes in precipitation-drought and deluge-persists beyond the extreme events. Chemical changes transcend such simple relations as increased salinity during dry periods because drought provides mechanisms for removal of salt by deflation and seepage to groundwater. Inundation of vegetation zones
Authors
J. W. LaBaugh, T. C. Winter, G.A. Swanson, D. Rosenberry
US Geological Survey Toxic Substances Hydrology Program: Proceedings of the technical meeting, Colorado Springs, Colorado, September 20-24, 1993
No abstract available.
Authors
D.W. Morganwalp, D. A. Aronson
Climatic and lake temperature data for Wetland P1, Cottonwood Lake Area, Stutsman County, North Dakota, 1982-87
Research on the hydrology of Wetland P1 and the Cottonwood Lake Area includes the study of evaporation. Presented here in a graphical format are those data collected during the open-water seasons of 1982-87 that were needed for energy- budget and mass-transfer evaporation studies. The data include air temperatures, water surface and lake-bottom temperatures, windspeed, radiation, humidity, and pre
Authors
Renee S. Parkhurst, A.M. Sturrock, D. O. Rosenberry, T. C. Winter
The interaction of groundwater with prairie pothole wetlands in the Cottonwood Lake area, east-central North Dakota 1979-90
No abstract available.
Authors
Thomas C. Winter, Donald O. Rosenberry
Evaluation of 11 equations for determining evaporation for a small lake in the North Central United States
Eleven equations for calculating evaporation were compared with evaporation determined by the energy budget method for Williams Lake, Minnesota. Data were obtained from instruments on a raft, on land near the lake, and at a weather station 60 km south of the lake. The comparisons were based on monthly values for the open-water periods of 5 years, a total of 22 months. A modified DeBruin-Keijman, P
Authors
Thomas C. Winter, Donald O. Rosenberry, A.M. Sturrock
Science and Products
Filter Total Items: 132
Hydrology of prairie pothole wetlands during drought and deluge: A 17-year study of the Cottonwood Lake wetland complex in North Dakota in the perspective of longer term measured and proxy hydrological records
From 1988 to 1992 the north-central plains of North America had a drought that was followed by a wet period that continues to the present (1997). Data on the hydrology of the Cottonwood Lake area (CWLA) collected for nearly 10 years before, and during, the recent dry and wet periods indicate that some prairie pothole wetlands served only a recharge function under all climate conditions. Transpirat
Authors
T. C. Winter, D. O. Rosenberry
Hydrologic functions of prairie wetlands
Wetlands in the prairie known as potholes or sloughs represent an ever-changing mosaic of surface waters interacting with the atmosphere, groundwater, and each other in a variety of ways. Studies of groups of adjacent wetlands in different parts of the glaciated North American prairie have enabled some connections to be made between hydrologic processes, biological communities, and use of these we
Authors
J. W. LaBaugh, T. C. Winter, D. O. Rosenberry
Evaporation from a small prairie wetland in the Cottonwood Lake Area, North Dakota - An energy-budget study
Evaporation from Wetland Pl in the Cottonwood Lake area of North Dakota, USA was determined by the energy-budget method for 1982-85 and 1987. Evaporation rates were as high as 0.672 cm day-1. Incoming solar radiation, incoming atmospheric radiation, and long-wave radiation emitted from the water body are the largest energy fluxes to and from the wetland. Because of the small heat storage of the wa
Authors
R.S. Parkhurst, T. C. Winter, D. O. Rosenberry, A.M. Sturrock
Watershed-scale research from many perspectives : the Interdisciplinary Research Initiative at the Shingobee River headwaters area, Minnesota
No abstract available.
Authors
D. O. Rosenberry
Hydrological and chemical estimates of the water balance of a closed-basin lake in north central Minnesota
Chemical mass balances for sodium, magnesium, chloride, dissolved organic carbon, and oxygen 18 were used to estimate groundwater seepage to and from Williams Lake, Minnesota, over a 15-month period, from April 1991 through June 1992. Groundwater seepage to the lake and seepage from the lake to groundwater were determined independently using a flow net approach using data from water table wells in
Authors
James W. LaBaugh, Thomas C. Winter, Donald O. Rosenberry, Paul F. Schuster, Michael M. Reddy, George R. Aiken
Dynamics of water-table fluctuations in an upland between two prairie-pothole wetlands in North Dakota
Data from a string of instrumented wells located on an upland of 55 m width between two wetlands in central North Dakota, USA, indicated frequent changes in water-table configuration following wet and dry periods during 5 years of investigation. A seasonal wetland is situated about 1.5 m higher than a nearby semipermanent wetland, suggesting an average ground water-table gradient of 0.02. However,
Authors
Donald O. Rosenberry, Thomas C. Winter
Hydrological and biogeochemical research in the Shingobee River headwaters area, north-central Minnesota
No abstract available.
Authors
Thomas C. Winter
Changes in atmospheric circulation patterns affect midcontinent wetlands sensitive to climate
Twenty-seven years of data from midcontinent wetlands indicate that the response of these wetlands to extremes in precipitation-drought and deluge-persists beyond the extreme events. Chemical changes transcend such simple relations as increased salinity during dry periods because drought provides mechanisms for removal of salt by deflation and seepage to groundwater. Inundation of vegetation zones
Authors
J. W. LaBaugh, T. C. Winter, G.A. Swanson, D. Rosenberry
US Geological Survey Toxic Substances Hydrology Program: Proceedings of the technical meeting, Colorado Springs, Colorado, September 20-24, 1993
No abstract available.
Authors
D.W. Morganwalp, D. A. Aronson
Climatic and lake temperature data for Wetland P1, Cottonwood Lake Area, Stutsman County, North Dakota, 1982-87
Research on the hydrology of Wetland P1 and the Cottonwood Lake Area includes the study of evaporation. Presented here in a graphical format are those data collected during the open-water seasons of 1982-87 that were needed for energy- budget and mass-transfer evaporation studies. The data include air temperatures, water surface and lake-bottom temperatures, windspeed, radiation, humidity, and pre
Authors
Renee S. Parkhurst, A.M. Sturrock, D. O. Rosenberry, T. C. Winter
The interaction of groundwater with prairie pothole wetlands in the Cottonwood Lake area, east-central North Dakota 1979-90
No abstract available.
Authors
Thomas C. Winter, Donald O. Rosenberry
Evaluation of 11 equations for determining evaporation for a small lake in the North Central United States
Eleven equations for calculating evaporation were compared with evaporation determined by the energy budget method for Williams Lake, Minnesota. Data were obtained from instruments on a raft, on land near the lake, and at a weather station 60 km south of the lake. The comparisons were based on monthly values for the open-water periods of 5 years, a total of 22 months. A modified DeBruin-Keijman, P
Authors
Thomas C. Winter, Donald O. Rosenberry, A.M. Sturrock