Final Project Memo - Assessment of Water Availability and Streamflow Characteristics in the southeastern United States
Dates
Date Reported
2016-05-24
Summary
Estimates of flows in the stream are critical to inform natural resource managers of the water availability for both human and ecological needs. Monitoring flow in the stream using a streamgage provides information about the amount and timing of surface water resources. However, not every stream has a streamgage and decisions about water resources may need to be made in a watershed where there is no flow information. Hydrologic models can be used to provide estimates of streamflow in the absence of streamflow information. These models depend upon available streamflow data for calibration, and can be very inaccurate without the use of those data. This research developed a method to group watersheds that are gaged with watersheds that [...]
Summary
Estimates of flows in the stream are critical to inform natural resource managers of the water availability for both human and ecological needs. Monitoring flow in the stream using a streamgage provides information about the amount and timing of surface water resources. However, not every stream has a streamgage and decisions about water resources may need to be made in a watershed where there is no flow information. Hydrologic models can be used to provide estimates of streamflow in the absence of streamflow information. These models depend upon available streamflow data for calibration, and can be very inaccurate without the use of those data. This research developed a method to group watersheds that are gaged with watersheds that are not gaged so that accurate estimates of water availability can be provided regionally. To accomplish this, various models, techniques, and data were used to group watersheds across the southeastern United States. This means that watersheds were not necessarily grouped by proximity to one another, but instead were grouped based on their response to climate and their landscape setting. This results in consistently developed regional estimates of water availability for current and potential future climate and land cover in the southeastern United States.
