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Anne Jefferson
Assistant Professor
OFFICE: 208 McEniry
PHONE: 704-687-5977
E-MAIL: ajeffe10@uncc.edu
HOMEPAGE: http://www.geoearth.uncc.edu/faculty/ajeffe10/
SHORT VITAE: Click Here

TEACHING AND RESEARCH INTERESTS:
• Hydrogeology
• Watershed Processes
• Groundwater-surface water interactions
• Water resources and climate change

DEGREES:
Ph.D. (2006) Geology, Oregon State University
M.S. (2002) Water Resources Science, University of Minnesota
B.A. (2001) Earth and Planetary Science, The Johns Hopkins University

PROFILE:
My process-based research lies at the intersection of hydrogeology, surface water hydrology, and geomorphology. My work includes contributions from field projects, GIS, time series analyses, stable isotopes, laboratory experiments, and modeling. I like to ask scientific questions that explore how watersheds work.

The interplay between geology, topography, and the resultant partitioning of water between different flowpaths can have a major influence on hydrograph characteristics and groundwater resources. My Ph.D. research focused on how high permeability basaltic lava flows in the Oregon Cascades control groundwater flowpaths, streamflow patterns, and drainage network evolution. I am currently studying how the drainage density of watersheds may affect hydrologic response and peak flow magnitudes. Drainage density is inversely related to permeability of a catchment, and so should give a useful map-based metric for predicting drought tolerance and flood risk in ungaged watersheds. I am also interested in how the permeability heterogeneity structure of a watershed influences hydrologic response to precipitation events and drought periods, and I plan to do field and modeling investigations of this problem.

In light of climate change and increasing demands on water resources, it is important to understand how changes in the magnitude and timing of regional water fluxes and severe storms will impact groundwater resources and streamflow patterns. In Oregon, I examined how groundwater mediated seasonal and inter-annual climate variability in a seasonally snow-covered watershed. Interestingly, groundwater actually heightened the sensitivity to long-term climate change. I am currently involved in a project looking at current and future glacier contributions to streamflow near Mt. Hood, Oregon. I am interested in how changing storm intensities in the southeastern United States will affect groundwater recharge, and how increased evapotranspiration from hotter summers will change aquifer levels. I will also continue to develop scientific questions that make use of the wealth of historical data on streamflows, precipitation, and groundwater.

If you have an interest in watersheds and groundwater and are looking for an enthusiastic advisor, I encourage you to contact me to discuss possibilities for graduate work.