James Kennedy is a Geographer with the Upper Midwest Water Science Center.
Current Projects
SPARROW Model watershed delination (SPARROW relates in-stream water-quality measurements to spatially referenced characteristics of watersheds, including contaminant sources and factors influencing terrestrial and stream transport)
FEMA - flood water inundation maps
Streamstats - basin delination (StreamStats is a Web-based tool that allows users to obtain streamflow statistics, drainage-basin characteristics, and other information for user-selected sites on streams)
Education and Certifications
GIS Professional Certificate, in progress, GIS Certification Institute
Certificate, Geographic Information Systems Graduate Program, UW-Madison, 2002
B.S. Soil Science-Natural Resources, Univeristy of Wisconsin-Madison, 1998
Certificate, Nelson Institute of Environmental Studies Program, UW-Madison, 1998
Science and Products
SPARROW modeling: Great Lakes, Mississippi River, Ohio River, and Red River Basins
SPARROW nutrient modeling: Mississippi/Atchafalaya River Basin (MARB)
SPARROW nutrient modeling: Binational (US/Canada) models
SPARROW modeling: Estimating nutrient, sediment, and dissolved solids transport
Estimating 1970-99 average annual groundwater recharge in Wisconsin using streamflow data
Flood of June 2008 in Southern Wisconsin
Estimation of shallow ground-water recharge in the Great Lakes basin
Science and Products
- Science
SPARROW modeling: Great Lakes, Mississippi River, Ohio River, and Red River Basins
SPARROW models for the Great Lakes, Ohio River, Upper Mississippi River, and Red River Basins predict long-term mean annual loads, yields, concentrations, and source contributions of water, nitrogen, phosphorus, and sediment throughout the Midwest.SPARROW nutrient modeling: Mississippi/Atchafalaya River Basin (MARB)
SPARROW models for the Mississippi/Atchafalaya River Basin(MARB) predict long-term average loads, concentrations, yields, and source contributions of water, nitrogen, phosphorus, and suspended sediment to the Gulf of Mexico.SPARROW nutrient modeling: Binational (US/Canada) models
SPARROW phosphorus and nitrogen models are being developed for the entire Great Lakes Basin and the Upper Midwest part of the U.S., and the Red and Assiniboine River Basin, as part of a Binational project between the USGS and the International Joint Commission (IJC) and National Research Council (NRC) of Canada.SPARROW modeling: Estimating nutrient, sediment, and dissolved solids transport
SPARROW (SPAtially Referenced Regression On Watershed attributes) models estimate the amount of a contaminant transported from inland watersheds to larger water bodies by linking monitoring data with information on watershed characteristics and contaminant sources. Interactive, online SPARROW mapping tools allow for easy access to explore relations between human activities, natural processes, and... - Publications
Estimating 1970-99 average annual groundwater recharge in Wisconsin using streamflow data
Average annual recharge in Wisconsin for the period 1970-99 was estimated using streamflow data from U.S. Geological Survey continuous-record streamflow-gaging stations and partial-record sites. Partial-record sites have discharge measurements collected during low-flow conditions. The average annual base flow of a stream divided by the drainage area is a good approximation of the recharge rate; thFlood of June 2008 in Southern Wisconsin
In June 2008, heavy rain caused severe flooding across southern Wisconsin. The floods were aggravated by saturated soils that persisted from unusually wet antecedent conditions from a combination of floods in August 2007, more than 100 inches of snow in winter 2007-08, and moist conditions in spring 2008. The flooding caused immediate evacuations and road closures and prolonged, extensive damagesEstimation of shallow ground-water recharge in the Great Lakes basin
This report presents the results of the first known integrated study of long-term average ground-water recharge to shallow aquifers (generally less than 100 feet deep) in the United States and Canada for the Great Lakes, upper St. Lawrence, and Ottawa River Basins. The approach used was consistent throughout the study area and allows direct comparison of recharge rates in disparate parts of the st