An acoustic Doppler current profiler is being used to measure discharge at Manatee Springs, Florida.
John Stamm
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
Science and Products
Historical Water-Use in Florida
Actual Evapotranspiration for Florida
CFWSC Strategic Science Plan - Communication, Information Management, and Science Support
CFWSC Strategic Science Plan - References Cited
CFWSC Strategic Science Plan - Programmatic Areas and Plans
CFWSC Strategic Plan - Priority Issues
CFWSC Strategic Plan - Introduction
CFWSC Strategic Science Plan
Water-Use in Puerto Rico
Water-Use in Florida
Chemistry of Uncontaminated Alluvial Deposits of the Cheyenne and Belle Fourche Rivers, South Dakota
Webinar: Application of High Resolution Climate Models to Benefit Avian Conservation in the Prairie Pothole Region, Northern Great Plains
Change factors to derive projected future precipitation depth-duration-frequency (DDF) curves at 174 National Oceanic and Atmospheric Administration (NOAA) Atlas 14 stations in central and south Florida
Change factors to derive future precipitation depth-duration-frequency (DDF) curves at 174 National Oceanic and Atmospheric Administration (NOAA) Atlas 14 stations in central and south Florida
Development of projected depth-duration frequency curves (2050–89) for south Florida
Aligning climate models with stakeholder needs: Advances in communicating future rainfall uncertainties for south Florida decision makers
Assessment of uncertainty in multi-model means of downscaled south Florida precipitation for projected (2019-2099) climate
Arsenic geochemistry of alluvial sediments and pore waters affected by mine tailings along the Belle Fourche and Cheyenne River floodplains
Shoreline erosion at selected areas along Lake Sharpe on the Lower Brule Reservation in South Dakota, 1966–2015
Sources of groundwater and characteristics of surface-water recharge at Bell, White, and Suwannee Springs, Florida, 2012–13
Modern (1992–2011) and projected (2012–99) peak snowpack and May–July runoff for the Fort Peck Lake and Lake Sakakawea watersheds in the Upper Missouri River Basin
Climate and streamflow characteristics for selected streamgages in eastern South Dakota, water years 1945–2013
Effects of projected climate (2011–50) on karst hydrology and species vulnerability—Edwards aquifer, south-central Texas, and Madison aquifer, western South Dakota
Historical and projected climate (1901–2050) and hydrologic response of karst aquifers, and species vulnerability in south-central Texas and western South Dakota
Fluvial sediment fingerprinting: literature review and annotated bibliography
Trends in annual, seasonal, and monthly streamflow characteristics at 227 streamgages in the Missouri River watershed, water years 1960-2011
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.
Science and Products
Historical Water-Use in Florida
Actual Evapotranspiration for Florida
CFWSC Strategic Science Plan - Communication, Information Management, and Science Support
CFWSC Strategic Science Plan - References Cited
CFWSC Strategic Science Plan - Programmatic Areas and Plans
CFWSC Strategic Plan - Priority Issues
CFWSC Strategic Plan - Introduction
CFWSC Strategic Science Plan
Water-Use in Puerto Rico
Water-Use in Florida
Chemistry of Uncontaminated Alluvial Deposits of the Cheyenne and Belle Fourche Rivers, South Dakota
Webinar: Application of High Resolution Climate Models to Benefit Avian Conservation in the Prairie Pothole Region, Northern Great Plains
Change factors to derive projected future precipitation depth-duration-frequency (DDF) curves at 174 National Oceanic and Atmospheric Administration (NOAA) Atlas 14 stations in central and south Florida
Change factors to derive future precipitation depth-duration-frequency (DDF) curves at 174 National Oceanic and Atmospheric Administration (NOAA) Atlas 14 stations in central and south Florida
Development of projected depth-duration frequency curves (2050–89) for south Florida
Aligning climate models with stakeholder needs: Advances in communicating future rainfall uncertainties for south Florida decision makers
Assessment of uncertainty in multi-model means of downscaled south Florida precipitation for projected (2019-2099) climate
Arsenic geochemistry of alluvial sediments and pore waters affected by mine tailings along the Belle Fourche and Cheyenne River floodplains
Shoreline erosion at selected areas along Lake Sharpe on the Lower Brule Reservation in South Dakota, 1966–2015
Sources of groundwater and characteristics of surface-water recharge at Bell, White, and Suwannee Springs, Florida, 2012–13
Modern (1992–2011) and projected (2012–99) peak snowpack and May–July runoff for the Fort Peck Lake and Lake Sakakawea watersheds in the Upper Missouri River Basin
Climate and streamflow characteristics for selected streamgages in eastern South Dakota, water years 1945–2013
Effects of projected climate (2011–50) on karst hydrology and species vulnerability—Edwards aquifer, south-central Texas, and Madison aquifer, western South Dakota
Historical and projected climate (1901–2050) and hydrologic response of karst aquifers, and species vulnerability in south-central Texas and western South Dakota
Fluvial sediment fingerprinting: literature review and annotated bibliography
Trends in annual, seasonal, and monthly streamflow characteristics at 227 streamgages in the Missouri River watershed, water years 1960-2011
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.