Flow monitoring in Goodwater Creek Experimental Watershed started in 1971 at three nested watersheds ranging from 12 to 73 km 2 . Since then, runoff or stream flow has been measured at 14 plots, three fields, and 12 additional stream sites ranging from 0.0034 to 6067 km 2 in the Central Mississippi River Basin. Longterm data sets are important to document the changes resulting from anthropogenic and natural drivers. The data set presented here documents discharge across a range of catchment sizes in an area known for its high runoff potential. It constitutes the flow database of the Central Mississippi River Basin site of the Long-Term Agricultural Research network. Like the other sites of this network, data are accessible through the STEWARDS web interface (www.nrrig.mwa.ars.usda.gov/stewards/stewards. html). Here we (i) describe the data collection methods, (ii) document the data available at plot, field, and watershed scales, and (iii) provide the main characteristics of discharge. General characteristics of discharge per unit area for different cropping system management systems show that in this claypan soil setting, management and tillage of row crop systems do not affect surface flow during the growing season (April-October). Data from fields and stream sites show the dampening of peak flow values and lengthening of storm hydrographs caused by mixed land uses and longer times of concentration. Overall, stream flow accounts for a third of the precipitation, of which 80% is from surface runoff and 20% is from groundwater.
Long-Term Agroecosystem Research in the Central Mississippi River Basin: Goodwater Creek Experimental Watershed Flow DataClaire Baffaut,* E. John Sadler, and Fessehaie Ghidey S tream flow is affected by short-and long-term, natural (droughts or floods) and anthropogenic (land use and land cover changes, water withdrawals) factors. Increasing strain is being put on water resources, including more frequent droughts and floods, decreasing water quality, and increasing withdrawals for human consumption and agriculture. Correspondingly, there is a need for continued hydrologic studies in many regions of the world to improve our understanding of the hydrologic cycle and the impact of the different stressors (Gordon et al., 2008).