Acoustic Doppler current profiler, Manatee Strings, Florida
Acoustic Doppler current profiler, Manatee Strings, FloridaAn acoustic Doppler current profiler is being used to measure discharge at Manatee Springs, Florida.
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Deputy Center Director of the Caribbean-Florida Water Science Center, providing leadership and strategic direction to advance water-science research and operational excellence.
My interests are in geomorphology and related fields such as fluvial hydrology, sediment transport, stream and wetland restoration, Quaternary paleoclimate, and geographic information systems (GIS). I also have experience with computer simulations of global climate (using general circulation models, or GCMs), downscaling global-climate estimates to local scales (statistical climate models and dynamical models such as the Weather Research and Forecasting Model, or WRF), and modeling land-atmosphere interactions and feedbacks.
Education
Ph.D., Applied Geology, 1991, Kent State University
Dissertation: "Modeling Local Paleoclimates and Validation in the Southwest U.S."
M.S., Geology, 1981, The Pennsylvania State University
Thesis: "Geology at the Intersection of the Death Valley and Garlock Fault Zones, Southern Death Valley, California"
B.A., Honors in Geology, 1977, State University of New York, College at Oneonta
An acoustic Doppler current profiler is being used to measure discharge at Manatee Springs, Florida.
An acoustic Doppler current profiler is being used to measure discharge at Manatee Springs, Florida.
USGS Hydrologist David Bender using a photoionization detector on a split soil core from 15 to 20 feet for well EAFB FAC MW14_06, Fuels Area C, Ellsworth Air Force Base, South Dakota. The photoionization detector measures volatile organic compounds and other gases. In fall of 2013, the U.S. Geological Survey began a study in cooperation with the U.S.
USGS Hydrologist David Bender using a photoionization detector on a split soil core from 15 to 20 feet for well EAFB FAC MW14_06, Fuels Area C, Ellsworth Air Force Base, South Dakota. The photoionization detector measures volatile organic compounds and other gases. In fall of 2013, the U.S. Geological Survey began a study in cooperation with the U.S.
Drilling rig setup and drilling well EAFB FAC MW14_04 on Fuels Area C, Ellsworth Air Force Base, South Dakota. In fall of 2013, the U.S. Geological Survey began a study in cooperation with the U.S.
Drilling rig setup and drilling well EAFB FAC MW14_04 on Fuels Area C, Ellsworth Air Force Base, South Dakota. In fall of 2013, the U.S. Geological Survey began a study in cooperation with the U.S.
U.S. Geological Survey streamgage at Rhoads Fork near Rochford, South Dakota. Headwater springflow at the eastern edge of the Limestone Plateau provides flow to Rhoads Fork.
U.S. Geological Survey streamgage at Rhoads Fork near Rochford, South Dakota. Headwater springflow at the eastern edge of the Limestone Plateau provides flow to Rhoads Fork.
A South Dakota School of Mines and Technology student working for the USGS South Dakota Water Science Center installed a trail camera at the Lodge site in the fall of 2013 to take time-lapse images of shoreline erosion along the Missouri River near the town of Lower Brule on the Lower Brule Reservation.
A South Dakota School of Mines and Technology student working for the USGS South Dakota Water Science Center installed a trail camera at the Lodge site in the fall of 2013 to take time-lapse images of shoreline erosion along the Missouri River near the town of Lower Brule on the Lower Brule Reservation.
A South Dakota School of Mines and Technology student working for the USGS South Dakota Water Science Center installed a trail camera in the fall of 2013 on a pole at the Playground site to take time-lapse images of shoreline erosion along the Missouri River near the town of Lower Brule on the Lower Brule Reservation.
A South Dakota School of Mines and Technology student working for the USGS South Dakota Water Science Center installed a trail camera in the fall of 2013 on a pole at the Playground site to take time-lapse images of shoreline erosion along the Missouri River near the town of Lower Brule on the Lower Brule Reservation.
Sediment sampling was conducted in 2009-10 to document concentrations of metals in sediment in Quaternary-age fluvial deposits along the Cheyenne and Belle Fourche Rivers in western South Dakota.
Sediment sampling was conducted in 2009-10 to document concentrations of metals in sediment in Quaternary-age fluvial deposits along the Cheyenne and Belle Fourche Rivers in western South Dakota.
Sediment sampling was conducted in 2009-10 to document concentrations of metals in sediment in Quaternary-age fluvial deposits along the Cheyenne and Belle Fourche Rivers in western South Dakota.
Sediment sampling was conducted in 2009-10 to document concentrations of metals in sediment in Quaternary-age fluvial deposits along the Cheyenne and Belle Fourche Rivers in western South Dakota.
Stage plate at Arrowhead drainage basin upstream from Arrowhead Country Club in Rapid City, SD. Runoff from this drainage discharges into Rapid Creek. Stormwater runoff from urbanized lands is known to harm surface-water resources by increasing stream velocities, destroying natural habitat, and increasing pollutant loads in the receiving waters.
Stage plate at Arrowhead drainage basin upstream from Arrowhead Country Club in Rapid City, SD. Runoff from this drainage discharges into Rapid Creek. Stormwater runoff from urbanized lands is known to harm surface-water resources by increasing stream velocities, destroying natural habitat, and increasing pollutant loads in the receiving waters.
Stormwater runoff following a May 2008 storm event in the Arrowhead drainage basin in Rapid City, SD. Runoff from this drainage discharges into Rapid Creek. Stormwater runoff from urbanized lands is known to harm surface-water resources by increasing stream velocities, destroying natural habitat, and increasing pollutant loads in the receiving waters.
Stormwater runoff following a May 2008 storm event in the Arrowhead drainage basin in Rapid City, SD. Runoff from this drainage discharges into Rapid Creek. Stormwater runoff from urbanized lands is known to harm surface-water resources by increasing stream velocities, destroying natural habitat, and increasing pollutant loads in the receiving waters.
An acoustic Doppler current profiler is being used to measure discharge at Manatee Springs, Florida.
An acoustic Doppler current profiler is being used to measure discharge at Manatee Springs, Florida.
USGS Hydrologist David Bender using a photoionization detector on a split soil core from 15 to 20 feet for well EAFB FAC MW14_06, Fuels Area C, Ellsworth Air Force Base, South Dakota. The photoionization detector measures volatile organic compounds and other gases. In fall of 2013, the U.S. Geological Survey began a study in cooperation with the U.S.
USGS Hydrologist David Bender using a photoionization detector on a split soil core from 15 to 20 feet for well EAFB FAC MW14_06, Fuels Area C, Ellsworth Air Force Base, South Dakota. The photoionization detector measures volatile organic compounds and other gases. In fall of 2013, the U.S. Geological Survey began a study in cooperation with the U.S.
Drilling rig setup and drilling well EAFB FAC MW14_04 on Fuels Area C, Ellsworth Air Force Base, South Dakota. In fall of 2013, the U.S. Geological Survey began a study in cooperation with the U.S.
Drilling rig setup and drilling well EAFB FAC MW14_04 on Fuels Area C, Ellsworth Air Force Base, South Dakota. In fall of 2013, the U.S. Geological Survey began a study in cooperation with the U.S.
U.S. Geological Survey streamgage at Rhoads Fork near Rochford, South Dakota. Headwater springflow at the eastern edge of the Limestone Plateau provides flow to Rhoads Fork.
U.S. Geological Survey streamgage at Rhoads Fork near Rochford, South Dakota. Headwater springflow at the eastern edge of the Limestone Plateau provides flow to Rhoads Fork.
A South Dakota School of Mines and Technology student working for the USGS South Dakota Water Science Center installed a trail camera at the Lodge site in the fall of 2013 to take time-lapse images of shoreline erosion along the Missouri River near the town of Lower Brule on the Lower Brule Reservation.
A South Dakota School of Mines and Technology student working for the USGS South Dakota Water Science Center installed a trail camera at the Lodge site in the fall of 2013 to take time-lapse images of shoreline erosion along the Missouri River near the town of Lower Brule on the Lower Brule Reservation.
A South Dakota School of Mines and Technology student working for the USGS South Dakota Water Science Center installed a trail camera in the fall of 2013 on a pole at the Playground site to take time-lapse images of shoreline erosion along the Missouri River near the town of Lower Brule on the Lower Brule Reservation.
A South Dakota School of Mines and Technology student working for the USGS South Dakota Water Science Center installed a trail camera in the fall of 2013 on a pole at the Playground site to take time-lapse images of shoreline erosion along the Missouri River near the town of Lower Brule on the Lower Brule Reservation.
Sediment sampling was conducted in 2009-10 to document concentrations of metals in sediment in Quaternary-age fluvial deposits along the Cheyenne and Belle Fourche Rivers in western South Dakota.
Sediment sampling was conducted in 2009-10 to document concentrations of metals in sediment in Quaternary-age fluvial deposits along the Cheyenne and Belle Fourche Rivers in western South Dakota.
Sediment sampling was conducted in 2009-10 to document concentrations of metals in sediment in Quaternary-age fluvial deposits along the Cheyenne and Belle Fourche Rivers in western South Dakota.
Sediment sampling was conducted in 2009-10 to document concentrations of metals in sediment in Quaternary-age fluvial deposits along the Cheyenne and Belle Fourche Rivers in western South Dakota.
Stage plate at Arrowhead drainage basin upstream from Arrowhead Country Club in Rapid City, SD. Runoff from this drainage discharges into Rapid Creek. Stormwater runoff from urbanized lands is known to harm surface-water resources by increasing stream velocities, destroying natural habitat, and increasing pollutant loads in the receiving waters.
Stage plate at Arrowhead drainage basin upstream from Arrowhead Country Club in Rapid City, SD. Runoff from this drainage discharges into Rapid Creek. Stormwater runoff from urbanized lands is known to harm surface-water resources by increasing stream velocities, destroying natural habitat, and increasing pollutant loads in the receiving waters.
Stormwater runoff following a May 2008 storm event in the Arrowhead drainage basin in Rapid City, SD. Runoff from this drainage discharges into Rapid Creek. Stormwater runoff from urbanized lands is known to harm surface-water resources by increasing stream velocities, destroying natural habitat, and increasing pollutant loads in the receiving waters.
Stormwater runoff following a May 2008 storm event in the Arrowhead drainage basin in Rapid City, SD. Runoff from this drainage discharges into Rapid Creek. Stormwater runoff from urbanized lands is known to harm surface-water resources by increasing stream velocities, destroying natural habitat, and increasing pollutant loads in the receiving waters.