Donald O Rosenberry (Former Employee)
Science and Products
Filter Total Items: 130
Amphibian decline: An integrated analysis of multiple stressor effects
Capturing the attention and imagination of the public and the scientific community alike, the mysterious decline in amphibian populations drew scientists and resource managers from ecotoxicology and chemistry, ecology and field biology, conservation biology, and natural resource policy to a SETAC–Johnson Foundation workshop. Facilitating environmental stewardship, increasing capacity of the scienc
Mid-Holocene hydrologic model of the Shingobee watershed, Minnesota
A hydrologifc model of the Shingobee Watershed in north-central Minnesota was developed to reconstruct mid-Holocene paleo-lake levels for Williams Lake, a surface-water body located in the southern portion of the watershed. Hydrologic parameters for the model were first estimated in a calibration exercise using a 9-yr historical record (1990-1998) of climatic and hydrologic stresses. The model rep
Authors
S.K. Filby, Sharon M. Locke, M.A. Person, T. C. Winter, D. O. Rosenberry, J.L. Nieber, W.J. Gutowski, E. Ito
Water source to four U.S. wetlands: Implications for wetland management
Results of long-term field studies of wetlands in four different hydrogeologic and climatic settings in the United States indicate that each has considerably different sources of water, which affects their response to climate variability and land-use practices. A fen wetland in New Hampshire is supplied almost entirely by ground water that originates as seepage from Mirror Lake; therefore, stream
Authors
T. C. Winter, D. O. Rosenberry, D.C. Buso, D.A. Merk
Estimating methane production rates in bogs and landfills by deuterium enrichment of pore water
Raised bogs and municipal waste landfills harbor large populations of methanogens within their domed deposits of anoxic organic matter. Although the methane emissions from these sites have been estimated by various methods, limited data exist on the activity of the methanogens at depth. We therefore analyzed the stable isotopic signature of the pore waters in two raised bogs from northern Minnesot
Authors
D. I. Siegel, J. P. Chanton, P.H. Glaser, L.S. Chasar, D. O. Rosenberry
Plants as indicators of focused ground water discharge to a northern Minnesota lake
Determining the discharge of ground water to Shingobee Lake (66 ha), north-central Minnesota, is complicated by the presence of numerous springs situated adjacent to the lake and in the shallow portion of the lakebed. Springs first had to be located before these areas of more rapid discharge could be quantified. Two methods that rely on the distribution of aquatic plants are useful for locating sp
Authors
D. O. Rosenberry, Robert G. Striegl, D.C. Hudson
The use of principal component analysis for interpreting ground water hydrographs
Principal component analysis was used to define patterns in water table hydrographs at four small, lake-watershed research sites in the United States. The analysis provided insights into (1) characteristics of ground water recharge in different parts of the watersheds; (2) the effect of seepage from lakes on water table fluctuations; and (3) the effect of differences in geologic properties on wate
Authors
T. C. Winter, S.E. Mallory, T.R. Allen, D. O. Rosenberry
Unsaturated‐zone wedge beneath a large, natural lake
Lake Belle Taine (480 ha) in north central Minnesota receives on average 76,000 m3 d−1 of water from Little Sand Creek but has no outlet. Water seeps out of the lake, flows through glacial outwash, and discharges into three nearby lakes with stages 13–14 m lower than Belle Taine. Seepage‐meter data indicate water is seeping out of Belle Taine at velocities up to 263 cm d−1 . Hydraulic‐head measure
Authors
Donald O. Rosenberry
Hydrographs of lake stage, stream discharge, and hydraulic head in ground water for the Mirror Lake area, New Hampshire, 1979-1995
No abstract available.
Authors
T. C. Winter, D.C. Buso, R.S. Parkhurst, D. O. Rosenberry, M.L. Martinez
Movement of road salt to a small New Hampshire lake
Runoff of road salt from an interstate highway in New Hampshire has led to contamination of a lake and a stream that flows into the lake, in spite of the construction of a diversion berm to divert road salt runoff out of the lake drainage basin. Chloride concentration in the stream has increased by over an order of magnitude during the 23 yr since the highway was opened, and chloride concentration
Authors
D. O. Rosenberry, P.A. Bukaveckas, D.C. Buso, G.E. Likens, A.M. Shapiro, T. C. Winter
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
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
Science and Products
Filter Total Items: 130
Amphibian decline: An integrated analysis of multiple stressor effects
Capturing the attention and imagination of the public and the scientific community alike, the mysterious decline in amphibian populations drew scientists and resource managers from ecotoxicology and chemistry, ecology and field biology, conservation biology, and natural resource policy to a SETAC–Johnson Foundation workshop. Facilitating environmental stewardship, increasing capacity of the scienc
Mid-Holocene hydrologic model of the Shingobee watershed, Minnesota
A hydrologifc model of the Shingobee Watershed in north-central Minnesota was developed to reconstruct mid-Holocene paleo-lake levels for Williams Lake, a surface-water body located in the southern portion of the watershed. Hydrologic parameters for the model were first estimated in a calibration exercise using a 9-yr historical record (1990-1998) of climatic and hydrologic stresses. The model rep
Authors
S.K. Filby, Sharon M. Locke, M.A. Person, T. C. Winter, D. O. Rosenberry, J.L. Nieber, W.J. Gutowski, E. Ito
Water source to four U.S. wetlands: Implications for wetland management
Results of long-term field studies of wetlands in four different hydrogeologic and climatic settings in the United States indicate that each has considerably different sources of water, which affects their response to climate variability and land-use practices. A fen wetland in New Hampshire is supplied almost entirely by ground water that originates as seepage from Mirror Lake; therefore, stream
Authors
T. C. Winter, D. O. Rosenberry, D.C. Buso, D.A. Merk
Estimating methane production rates in bogs and landfills by deuterium enrichment of pore water
Raised bogs and municipal waste landfills harbor large populations of methanogens within their domed deposits of anoxic organic matter. Although the methane emissions from these sites have been estimated by various methods, limited data exist on the activity of the methanogens at depth. We therefore analyzed the stable isotopic signature of the pore waters in two raised bogs from northern Minnesot
Authors
D. I. Siegel, J. P. Chanton, P.H. Glaser, L.S. Chasar, D. O. Rosenberry
Plants as indicators of focused ground water discharge to a northern Minnesota lake
Determining the discharge of ground water to Shingobee Lake (66 ha), north-central Minnesota, is complicated by the presence of numerous springs situated adjacent to the lake and in the shallow portion of the lakebed. Springs first had to be located before these areas of more rapid discharge could be quantified. Two methods that rely on the distribution of aquatic plants are useful for locating sp
Authors
D. O. Rosenberry, Robert G. Striegl, D.C. Hudson
The use of principal component analysis for interpreting ground water hydrographs
Principal component analysis was used to define patterns in water table hydrographs at four small, lake-watershed research sites in the United States. The analysis provided insights into (1) characteristics of ground water recharge in different parts of the watersheds; (2) the effect of seepage from lakes on water table fluctuations; and (3) the effect of differences in geologic properties on wate
Authors
T. C. Winter, S.E. Mallory, T.R. Allen, D. O. Rosenberry
Unsaturated‐zone wedge beneath a large, natural lake
Lake Belle Taine (480 ha) in north central Minnesota receives on average 76,000 m3 d−1 of water from Little Sand Creek but has no outlet. Water seeps out of the lake, flows through glacial outwash, and discharges into three nearby lakes with stages 13–14 m lower than Belle Taine. Seepage‐meter data indicate water is seeping out of Belle Taine at velocities up to 263 cm d−1 . Hydraulic‐head measure
Authors
Donald O. Rosenberry
Hydrographs of lake stage, stream discharge, and hydraulic head in ground water for the Mirror Lake area, New Hampshire, 1979-1995
No abstract available.
Authors
T. C. Winter, D.C. Buso, R.S. Parkhurst, D. O. Rosenberry, M.L. Martinez
Movement of road salt to a small New Hampshire lake
Runoff of road salt from an interstate highway in New Hampshire has led to contamination of a lake and a stream that flows into the lake, in spite of the construction of a diversion berm to divert road salt runoff out of the lake drainage basin. Chloride concentration in the stream has increased by over an order of magnitude during the 23 yr since the highway was opened, and chloride concentration
Authors
D. O. Rosenberry, P.A. Bukaveckas, D.C. Buso, G.E. Likens, A.M. Shapiro, T. C. Winter
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
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