Donald O Rosenberry (Former Employee)
Science and Products
Filter Total Items: 132
Characterization of lake water and ground water movement in the littoral zone of Williams Lake, a closed-basin lake in North central Minnesota
Williams Lake, Minnesota is a closed‐basin lake that is a flow‐through system with respect to ground water. Ground‐water input represents half of the annual water input and most of the chemical input to the lake. Chemical budgets indicate that the lake is a sink for calcium, yet surficial sediments contain little calcium carbonate. Sediment pore‐water samplers (peepers) were used to characterize s
Authors
P. F. Schuster, M.M. Reddy, J. W. LaBaugh, R.S. Parkhurst, D. O. Rosenberry, T. C. Winter, Ronald C. Antweiler, W.E. Dean
Evaporation determined by the energy-budget method for Mirror Lake, New Hampshire
Evaporation was determined by the energy-budget method for Mirror Lake during the open water periods of 1982-1987. For all years, evaporation rates were low in spring and fall and highest during the summer. However, the times of highest evaporation rates varied during the 6 yr. Evaporation reached maximum rates in July for three of the years, in June for two of the years, and in August for one of
Authors
T. C. Winter, D.C. Buso, D. O. Rosenberry, G.E. Likens, A.M. Sturrock, D.P. Mau
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
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
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
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
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
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
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
Science and Products
Filter Total Items: 132
Characterization of lake water and ground water movement in the littoral zone of Williams Lake, a closed-basin lake in North central Minnesota
Williams Lake, Minnesota is a closed‐basin lake that is a flow‐through system with respect to ground water. Ground‐water input represents half of the annual water input and most of the chemical input to the lake. Chemical budgets indicate that the lake is a sink for calcium, yet surficial sediments contain little calcium carbonate. Sediment pore‐water samplers (peepers) were used to characterize s
Authors
P. F. Schuster, M.M. Reddy, J. W. LaBaugh, R.S. Parkhurst, D. O. Rosenberry, T. C. Winter, Ronald C. Antweiler, W.E. Dean
Evaporation determined by the energy-budget method for Mirror Lake, New Hampshire
Evaporation was determined by the energy-budget method for Mirror Lake during the open water periods of 1982-1987. For all years, evaporation rates were low in spring and fall and highest during the summer. However, the times of highest evaporation rates varied during the 6 yr. Evaporation reached maximum rates in July for three of the years, in June for two of the years, and in August for one of
Authors
T. C. Winter, D.C. Buso, D. O. Rosenberry, G.E. Likens, A.M. Sturrock, D.P. Mau
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
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
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
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
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
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
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