HR: 0800h
AN: H31C-0388 INVITED     [Abstracts]
TI: Yazoo River Basin (Lower Mississippi River) Hydrologic Observatory
AU: * Cheng, A
EM: acheng@olemiss.edu
AF: University of Mississippi, Civil Engineering, Carrier 203, University, MS 38677 United States
AU: Davidson, G
EM: davidson@olemiss.edu
AF: University of Mississippi, Geology and Geological Engineering, Carrier 118, University, MS 38677 United States
AU: Altinakar, M
EM: altinakar@ncche.olemiss.edu
AF: University of Mississippi, Nat. Center for Compuational Hydroscience, Carrier 102, University, MS 38677 United States
AU: Holt, R
EM: rmholt@olemiss.edu
AF: University of Mississippi, Geology and Geological Engineering, Carrier 118, University, MS 38677 United States
AB: The proposed Yazoo River Basin Hydrologic Observatory consists of the 34,000 square km Yazoo River watershed in northwestern Mississippi and a 320 km segment of the Mississippi River separated from the watershed by a manmade levee. Discharge from the basin flows from the Yazoo River into the Mississippi River north of Vicksburg, MS. Major streams within the basin include the Yazoo, Tallahatchie, Yalobusha, Coldwater, Yocona, and Big Sunflower Rivers. Four large flood control reservoirs (Arkabutla, Enid, Sardis, and Grenada) and two national forests (Delta and Holly Springs) are also located within the basin. The watershed is divided between upland forested hills and intensively cultivated lowlands. The lowland area, locally known as the "Delta", lies on the ancestral floodplain of the Mississippi River. Flooding by the Mississippi River was once a common event, but is now limited by the levee system. Abundant wetlands occupy abandoned stream channels throughout the Delta. The Yazoo River Basin has many unique features that make it an attractive site for an Hydrologic Observatory. Example features and issues of scientific interest include: 1) Extensive system of levees which have altered recharge to the regional aquifer, shifted population centers, and created backwater flooding areas. 2) Abundant wetlands with a century-long history of response to agricultural sediment and chemical fluxes. 3) Erosion of upland streams, and stream sediment loads that are the highest in the nation. 4) Groundwater mining in spite of abundant precipitation due to a regional surface clay layer that limits infiltration. 5) A history of agricultural Best Management Practices enabling evaluation of the effectiveness of such measures. 6) Large scale catfish farming with heavy reliance on groundwater. 7) Near enough to the Gulf coast to be impacted by hurricane events. 8) Already existing network of monitoring stations for stream flow, sediment-load, and weather, including complete coverage by four NWS NEXRAD Doppler radar systems. 9) Long history of national interest and investment including flood control projects, wetland restoration, and dredging by the US Army Corps of Engineers, an intensively instrumented national watershed observatory by the USDA Agricultural Research Service in Goodwin Creek, and numerous other projects by over 20 federal and state agencies. 10) Availability of a 2300 square meter research facility within the watershed for housing research and administrative activities.
DE: 1800 HYDROLOGY
DE: 1848 Networks
SC: Hydrology [H]
MN: 2004 AGU Fall Meeting