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(1978)
A community analysis of the piedmont deciduous forest of Panola Mountain State Conservation
H. Meerveld, J. McDonnell (2006)
On the interrelations between topography, soil depth, soil moisture, transpiration rates and species distribution at the hillslope scaleAdvances in Water Resources, 29
(1999)
Tracers and hydrometric study of preferential flow in large undisturbed soil cores from the Georgia Piedmont, USA, Hydrol. Processes
(1978)
A community analysis of the piedmont deciduous forest of Panola Mountain State Conservation Park
J. McDonnell, J. Freer, R. Hooper, C. Kendall, D. Burns, K. Beven, J. Peters (1996)
NEW METHOD DEVELOPED FOR STUDYING FLOW ON HILLSLOPESEos, Transactions American Geophysical Union, 77
H. Meerveld, N. Peters, J. McDonnell (2007)
Effect of bedrock permeability on subsurface stormflow and the water balance of a trenched hillslope at the Panola Mountain Research Watershed, Georgia, USAHydrological Processes, 21
(1998)
Spatial modeling of soil depth and landscape variability in a small forested catchment
Department of Forestry and Environmental Resources
J. Mcintosh, J. McDonnell, N. Peters (1999)
Tracer and hydrometric study of preferential flow in large undisturbed soil cores from the Georgia Piedmont, USAHydrological Processes, 13
J. Freer, J. McDonnell, K. Beven, D. Brammer, D. Burns, R. Hooper, C. Kendal (1997)
Hydrological processes—Letters. Topographic controls on subsurface storm flow at the hillslope scale for two hydrologically distinct small catchmetnsHydrological Processes, 11
J. Freer, J. McDonnell, K. Beven, D. Brammer, D. Burns, R. Hooper, C. Kendal (1997)
TOPOGRAPHIC CONTROLS ON SUBSURFACE STORM FLOWAT THE HILLSLOPE SCALE FOR TWO HYDROLOGICALLY DISTINCT SMALL CATCHMENTS
H. Lins (1994)
Recent directions taken in water, energy, and biogeochemical budgets researchEos, Transactions American Geophysical Union, 75
(1999)
Tracers and hydrometric study of preferential flow in large undisturbed soil cores from the Georgia Piedmont
(2007)
Rainfall threshold for hillslope outflow: An emergent property of flow path connectivity, Hydrol
K. Beven (2006)
Searching for the Holy Grail of Scientific Hydrology: Qt= H(S?R?)A as closure
T. Huntington, R. Hooper, N. Peters, T. Bullen, C. Kendall (1993)
Water, energy, and biogeochemical budgets investigation at Panola Mountain research watershed, Stockbridge, Georgia; a research plan
(1999)
Revision of stratigraphic nomenclature in the Atlanta, Athens, and Cartersville 30 Â 60 quadrangles
(2006)
Searching for the holy grail of scientific hydrology: Q t = Hð ! S
D. Burns, J. McDonnell, R. Hooper, N. Peters, J. Freer, C. Kendall, K. Beven (2001)
Quantifying contributions to storm runoff through end‐member mixing analysis and hydrologic measurements at the Panola Mountain Research Watershed (Georgia, USA)Hydrological Processes, 15
M. Hoover, C. Hursh (1943)
Influence of topography and soil‐depth on runoff from forest landEos, Transactions American Geophysical Union, 24
(1993)
Water, energy, and biogeochemical budgets investigation
(1999)
The hydrochemistry of stormflow in a forested Piedmont catchment
(2005)
Subsurface stormflow, in Encyclopedia
H. Meerveld, J. McDonnell (2006)
Threshold relations in subsurface stormflow: 2. The fill and spill hypothesisWater Resources Research, 42
(1903)
Quantifying contributions to storm runoff using end-member mixing analysis and hydrologic measurements at the Panola Mountain Research Watershed
D. Burns, R. Hooper, J. McDonnell, J. Freer, C. Kendall, K. Beven (1998)
Base cation concentrations in subsurface flow from a forested hillslope: The role of flushing frequencyWater Resources Research, 34
(1990)
Local climatological data, annual summary with comparative data
(2006)
Searching for the holy grail of scientific hydrology: Qt = Hð!S; R;DtÞ!A as closure, Hydrol
N. Peters, James Freer, B. Aulenbach (2003)
Hydrological Dynamics of the Panola Mountain Research Watershed, GeorgiaGroundwater, 41
B. Welch (1992)
The structureObject Magazine archive, 1
Hoover Hoover, Hursh Hursh (1943)
Influence of topography and soil depth on runoff from forest landEos Trans. AGU, 24
T. Uchida, I. Meerveld, J. McDonnell (2005)
The role of lateral pipe flow in hillslope runoff response: an intercomparison of non-linear hillslope responseJournal of Hydrology, 311
J. Freer, Jeffery McDonnell, Keith Beven, Norman Peters, Douglas Burns, Richard Hooper, B. Aulenbach, Carol Kendall (2002)
The role of bedrock topography on subsurface storm flowWater Resources Research, 38
(1999)
Revision of stratigraphic nomenclature in the Atlanta, Athens, and Cartersville
Beven (2006)
Searching for the holy grail of scientific hydrology: Qt = H( as closureHydrol. Earth Syst. Sci., 10
R. Cappellato, N. Peters, H. Ragsdale (1993)
Acidic atmospheric deposition and canopy interactions of adjacent deciduous and coniferous forests in the Georgia PiedmontCanadian Journal of Forest Research, 23
A. White, A. Blum, M. Schulz, T. Huntington, N. Peters, D. Stonestrom (2001)
Chemical weathering of the Panola Granite: Solute and regolith elemental fluxes and the weathering rate of biotite
McDonnell McDonnell, Freer Freer, Hooper Hooper, Kendall Kendall, Burns Burns, Beven Beven, Peters Peters (1996)
New method developed for studying flow in hillslopesEos Trans. AGU, 77
H. Meerveld, Jeffrey McDonnell (2006)
Threshold relations in subsurface stormflow: 1. A 147‐storm analysis of the Panola hillslopeWater Resources Research, 42
(1999)
Revision of stratigraphic nomenclature in the Atlanta, Athens, and Cartersville 30
Lins Lins (1994)
Recent directions taken in water, energy and biogeochemical budgets researchEos Trans. AGU, 75
(2005)
Subsurface stormflow
P. Lehmann, P. Lehmann, Christoph Hinz, G. McGrath, H. Meerveld, H. Meerveld, J. McDonnell, J. McDonnell
Hydrology and Earth System Sciences Rainfall Threshold for Hillslope Outflow: an Emergent Property of Flow Pathway Connectivity
(1993)
Water, energy, and biogeochemical budgets investigation at Panola Mountain Research Watershed
Although many hillslope hydrologic investigations have been conducted in different climate, topographic, and geologic settings, subsurface stormflow remains a poorly characterized runoff process. Few, if any, of the existing data sets from these hillslope investigations are available for use by the scientific community for model development and validation or conceptualization of subsurface stormflow. We present a high‐resolution spatial and temporal rainfall‐runoff data set generated from the Panola Mountain Research Watershed trenched experimental hillslope. The data set includes surface and subsurface (bedrock surface) topographic information and time series of lateral subsurface flow at the trench, rainfall, and subsurface moisture content (distributed soil moisture content and groundwater levels) from January to June 2002.
Water Resources Research – Wiley
Published: Jun 1, 2008
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