High pressure dominated the southern half of the contiguous U.S. (CONUS) during this U.S. Drought Monitor (USDM) week. Upper-level weather systems tracked across the U.S.-Canadian border, dragging surface lows and fronts along with them. The frontal systems tapped Gulf of Mexico moisture to drop locally heavy rain across parts of the Plains to Midwest, while convective thunderstorms peppered coastal areas of the Gulf. The high-pressure ridge inhibited precipitation across much of the southern Plains to Southeast, and across most of the West. It also kept temperatures unusually hot, with daily maximums exceeding 90 degrees F across the South throughout the week and across much of the West for most of the week. The excessive heat spread into the northern Plains, Midwest, and into the Northeast as the week wore on. The persistent heat increased evapotranspiration, which dried soils and stressed crops and other vegetation. The locally heavy rains brought temporary relief from the heat and dryness, but only for those areas in the Plains and Midwest lucky enough to receive the rain.