Donald O Rosenberry (Former Employee)
Science and Products
Filter Total Items: 132
Reply to comment by J. Szilagyi on "Comparison of 15 evaporation methods applied to a small mountain lake in the northeastern USA" [J. Hydrol. 340 (3-4) (2007) 149-166]
[No abstract available]
Authors
D. O. Rosenberry, T. C. Winter, D.C. Buso, G.E. Likens
A seepage meter designed for use in flowing water
Seepage meters provide one of the most direct means to measure exchange of water across the sediment-water interface, but they generally have been unsuitable for use in fluvial settings. Although the seepage bag can be placed inside a rigid container to minimize velocity head concerns, the seepage cylinder installed in the sediment bed projects into and disrupts the flow field, altering both the l
Authors
D. O. Rosenberry
Comparison of 15 evaporation methods applied to a small mountain lake in the northeastern USA
Few detailed evaporation studies exist for small lakes or reservoirs in mountainous settings. A detailed evaporation study was conducted at Mirror Lake, a 0.15 km2 lake in New Hampshire, northeastern USA, as part of a long-term investigation of lake hydrology. Evaporation was determined using 14 alternate evaporation methods during six open-water seasons and compared with values from the Bowen-rat
Authors
Donald O. Rosenberry, Thomas C. Winter, D.C. Buso, G.E. Likens
Hydrologic response of the Crow Wing Watershed, Minnesota, to mid-Holocene climate change
In this study, we have integrated a suite of Holocene paleoclimatic proxies with mathematical modeling in an attempt to obtain a comprehensive picture of how watersheds respond to past climate change. A three-dimensional surface-water-groundwater model was developed to assess the effects of mid-Holocene climate change on water resources within the Crow Wing Watershed, Upper Mississippi Basin in no
Authors
M. Person, P. Roy, H. Wright, W. Gutowski, E. Ito, T. Winter, D. Rosenberry, D. Cohen
Heat transport in the Red Lake Bog, Glacial Lake Agassiz Peatlands
We report the results of an investigation on the processes controlling heat transport in peat under a large bog in the Glacial Lake Agassiz Peatlands. For 2 years, starting in July 1998, we recorded temperature at 12 depth intervals from 0 to 400 cm within a vertical peat profile at the crest of the bog at sub‐daily intervals. We also recorded air temperature 1 m above the peat surface. We calcula
Authors
J.M. McKenzie, D. I. Siegel, Donald O. Rosenberry, P.H. Glaser, Clifford I. Voss
Use of carboxylated microspheres to assess transport potential of Cryptosporidium parvum oocysts at the Russian River water supply facility, Sonoma County, California
Carboxylated microspheres were employed as surrogates to assess the transport potential of Cryptosporidium parvumoocysts during forced- and natural-gradient tests conducted in July and October 2004. The tests involved poorly-sorted, near-surface sediments where groundwater is pumped from an alluvial aquifer underlying the Russian River, Sonoma County, CA. In an off channel infiltration basin and w
Authors
David W. Metge, Ronald W. Harvey, Robert Anders, Donald O. Rosenberry, Donald Seymour, Jay Jasperse
A system for calibrating seepage meters used to measure flow between ground water and surface water
A system has been developed for generating controlled rates of seepage across the sediment-water interface representing flow between ground water and surface water. The seepage- control system facilitates calibration and testing of seepage measurement devices commonly called seepage meters. Two slightly different seepage-control systems were evaluated. Both designs make use of a 1.5-m-diameter by
Authors
Donald O. Rosenberry, Michael A. Menheer
The significance of ground water to the accumulation of iron and manganese in the sediments of two hydrologically distinct lakes in north‐central Minnesota: A geological perspective
Williams and Shingobee lakes are at opposite ends of the local ground water flow system in the Shingobee River Headwaters Area (SRHA) in north‐central Minnesota. Williams Lake, situated near the highest point in the flow system, has no surface inlet or outlet, and ground water and precipitation are the only sources of water. Shingobee Lake, situated at the lowest point in the flow system, has the
Authors
Walter E. Dean, Brian Neff, Donald O. Rosenberry, Thomas C. Winter, Renee S. Parkhurst
Groundwater-supported evapotranspiration within glaciated watersheds under conditions of climate change
This paper analyzes the effects of geology and geomorphology on surface-water/-groundwater interactions, evapotranspiration, and recharge under conditions of long-term climatic change. Our analysis uses hydrologic data from the glaciated Crow Wing watershed in central Minnesota, USA, combined with a hydrologic model of transient coupled unsaturated/saturated flow (HYDRAT2D). Analysis of historical
Authors
D. Cohen, M. Person, R. Daannen, S. Locke, D. Dahlstrom, V. Zabielski, T. C. Winter, D. O. Rosenberry, H. Wright, E. Ito, J.L. Nieber, W.J. Gutowski
Flow path oscillations in transient ground-water simulations of large peatland systems
Transient numerical simulations of the Glacial Lake Agassiz Peatland near the Red Lakes in Northern Minnesota were constructed to evaluate observed reversals in vertical ground-water flow. Seasonal weather changes were introduced to a ground-water flow model by varying evapotranspiration and recharge over time. Vertical hydraulic reversals, driven by changes in recharge and evapotranspiration were
Authors
A.S. Reeve, R. Evensen, P.H. Glaser, D. I. Siegel, D. Rosenberry
The hydrology of northern peatlands as affected by biogenic gas: Current developments and research needs
Recent research indicates that accumulation and release of biogenic gas from northern peatlands may substantially affect future climate. Sudden release of free-phase gas bubbles into the atmosphere may preclude the conversion of methane to carbon dioxide in the uppermost oxic layer of the peat, resulting in greater contribution of methane to the atmosphere than is currently estimated. The hydrolog
Authors
D. O. Rosenberry, P.H. Glaser, D. I. Siegel
Coastal groundwater/surface-water interactions: a Great Lakes case study
Key similarities exist between marine and Great Lakes coastal environments. Water and nutrient fluxes across lakebeds in the Great Lakes are influenced by seiche and wind set-up and set-down, analogous to tidal influence in marine settings. Groundwater/surface-water interactions also commonly involve a saline-fresh water interface, although in the Great-Lakes cases, it is groundwater that is commo
Authors
Brian P. Neff, Sheridan K. Haack, Donald O. Rosenberry, Jacqueline F. Savino, Scott C. Lundstrom
Science and Products
Filter Total Items: 132
Reply to comment by J. Szilagyi on "Comparison of 15 evaporation methods applied to a small mountain lake in the northeastern USA" [J. Hydrol. 340 (3-4) (2007) 149-166]
[No abstract available]
Authors
D. O. Rosenberry, T. C. Winter, D.C. Buso, G.E. Likens
A seepage meter designed for use in flowing water
Seepage meters provide one of the most direct means to measure exchange of water across the sediment-water interface, but they generally have been unsuitable for use in fluvial settings. Although the seepage bag can be placed inside a rigid container to minimize velocity head concerns, the seepage cylinder installed in the sediment bed projects into and disrupts the flow field, altering both the l
Authors
D. O. Rosenberry
Comparison of 15 evaporation methods applied to a small mountain lake in the northeastern USA
Few detailed evaporation studies exist for small lakes or reservoirs in mountainous settings. A detailed evaporation study was conducted at Mirror Lake, a 0.15 km2 lake in New Hampshire, northeastern USA, as part of a long-term investigation of lake hydrology. Evaporation was determined using 14 alternate evaporation methods during six open-water seasons and compared with values from the Bowen-rat
Authors
Donald O. Rosenberry, Thomas C. Winter, D.C. Buso, G.E. Likens
Hydrologic response of the Crow Wing Watershed, Minnesota, to mid-Holocene climate change
In this study, we have integrated a suite of Holocene paleoclimatic proxies with mathematical modeling in an attempt to obtain a comprehensive picture of how watersheds respond to past climate change. A three-dimensional surface-water-groundwater model was developed to assess the effects of mid-Holocene climate change on water resources within the Crow Wing Watershed, Upper Mississippi Basin in no
Authors
M. Person, P. Roy, H. Wright, W. Gutowski, E. Ito, T. Winter, D. Rosenberry, D. Cohen
Heat transport in the Red Lake Bog, Glacial Lake Agassiz Peatlands
We report the results of an investigation on the processes controlling heat transport in peat under a large bog in the Glacial Lake Agassiz Peatlands. For 2 years, starting in July 1998, we recorded temperature at 12 depth intervals from 0 to 400 cm within a vertical peat profile at the crest of the bog at sub‐daily intervals. We also recorded air temperature 1 m above the peat surface. We calcula
Authors
J.M. McKenzie, D. I. Siegel, Donald O. Rosenberry, P.H. Glaser, Clifford I. Voss
Use of carboxylated microspheres to assess transport potential of Cryptosporidium parvum oocysts at the Russian River water supply facility, Sonoma County, California
Carboxylated microspheres were employed as surrogates to assess the transport potential of Cryptosporidium parvumoocysts during forced- and natural-gradient tests conducted in July and October 2004. The tests involved poorly-sorted, near-surface sediments where groundwater is pumped from an alluvial aquifer underlying the Russian River, Sonoma County, CA. In an off channel infiltration basin and w
Authors
David W. Metge, Ronald W. Harvey, Robert Anders, Donald O. Rosenberry, Donald Seymour, Jay Jasperse
A system for calibrating seepage meters used to measure flow between ground water and surface water
A system has been developed for generating controlled rates of seepage across the sediment-water interface representing flow between ground water and surface water. The seepage- control system facilitates calibration and testing of seepage measurement devices commonly called seepage meters. Two slightly different seepage-control systems were evaluated. Both designs make use of a 1.5-m-diameter by
Authors
Donald O. Rosenberry, Michael A. Menheer
The significance of ground water to the accumulation of iron and manganese in the sediments of two hydrologically distinct lakes in north‐central Minnesota: A geological perspective
Williams and Shingobee lakes are at opposite ends of the local ground water flow system in the Shingobee River Headwaters Area (SRHA) in north‐central Minnesota. Williams Lake, situated near the highest point in the flow system, has no surface inlet or outlet, and ground water and precipitation are the only sources of water. Shingobee Lake, situated at the lowest point in the flow system, has the
Authors
Walter E. Dean, Brian Neff, Donald O. Rosenberry, Thomas C. Winter, Renee S. Parkhurst
Groundwater-supported evapotranspiration within glaciated watersheds under conditions of climate change
This paper analyzes the effects of geology and geomorphology on surface-water/-groundwater interactions, evapotranspiration, and recharge under conditions of long-term climatic change. Our analysis uses hydrologic data from the glaciated Crow Wing watershed in central Minnesota, USA, combined with a hydrologic model of transient coupled unsaturated/saturated flow (HYDRAT2D). Analysis of historical
Authors
D. Cohen, M. Person, R. Daannen, S. Locke, D. Dahlstrom, V. Zabielski, T. C. Winter, D. O. Rosenberry, H. Wright, E. Ito, J.L. Nieber, W.J. Gutowski
Flow path oscillations in transient ground-water simulations of large peatland systems
Transient numerical simulations of the Glacial Lake Agassiz Peatland near the Red Lakes in Northern Minnesota were constructed to evaluate observed reversals in vertical ground-water flow. Seasonal weather changes were introduced to a ground-water flow model by varying evapotranspiration and recharge over time. Vertical hydraulic reversals, driven by changes in recharge and evapotranspiration were
Authors
A.S. Reeve, R. Evensen, P.H. Glaser, D. I. Siegel, D. Rosenberry
The hydrology of northern peatlands as affected by biogenic gas: Current developments and research needs
Recent research indicates that accumulation and release of biogenic gas from northern peatlands may substantially affect future climate. Sudden release of free-phase gas bubbles into the atmosphere may preclude the conversion of methane to carbon dioxide in the uppermost oxic layer of the peat, resulting in greater contribution of methane to the atmosphere than is currently estimated. The hydrolog
Authors
D. O. Rosenberry, P.H. Glaser, D. I. Siegel
Coastal groundwater/surface-water interactions: a Great Lakes case study
Key similarities exist between marine and Great Lakes coastal environments. Water and nutrient fluxes across lakebeds in the Great Lakes are influenced by seiche and wind set-up and set-down, analogous to tidal influence in marine settings. Groundwater/surface-water interactions also commonly involve a saline-fresh water interface, although in the Great-Lakes cases, it is groundwater that is commo
Authors
Brian P. Neff, Sheridan K. Haack, Donald O. Rosenberry, Jacqueline F. Savino, Scott C. Lundstrom