Widespread rain and cooler than normal temperatures across the region led to one-category improvements in southeast Tennessee, west-central Oklahoma, and much of Texas. Improvements in Tennessee are supported by precipitation, streamflow, and soil moisture. In Oklahoma, the northern edge of abnormal dryness was trimmed as precipitation deficits in this area have been erased out to six months. Many of the drought-affected areas in Texas saw weekly precipitation that exceeded 300 to 600 percent of normal, resulting in the elimination of extreme drought (D3) in the northern part of the state and overall reductions to the other categories. The southern part of the state also saw broad areas of improvement. Note that the designation “SL” was added to the southwest region to reflect the short- and long-term nature of the precipitation deficits and impacts.