As a result, drought and abnormal dryness expanded across much of the western half of the region, especially from western New Jersey through Pennsylvania and New York, as well as northern Virginia and eastern West Virginia. More generally over the last few weeks, especially across the western half of the Northeast, streamflows and soil moisture are very low, amid unusually hot temperatures and high evaporative demand for this time of year. Coastal areas tended to be cooler than normal this week, with isolated spots coming in 4 to 6 degrees below normal. Temperatures were mostly above normal across the western half of the region, with localized readings ranging from 4 to 6 degrees warmer than normal. Pennsylvania, New York, Maryland, New Jersey, Delaware and southern New England saw primarily dry weather this week. Degradations were made in a few parts of western Montana and northwest Washington, where precipitation deficits mounted amid declining soil moisture and streamflow. In the West, some minor improvements occurred in parts of Nevada, Utah and Idaho, where high streamflows and large precipitation amounts from the winter into May led to a reassessment of conditions. Widespread degradations occurred in the Midwest and western portions of the Northeast, amid very dry and warm recent weather. Heavy rains in the central and southern Florida Peninsula also led to improvements to ongoing drought and abnormal dryness in the southwest Florida Peninsula. Heavy rains fell this week across some of the western parts of the Central and Southern Great Plains, especially in the Texas Panhandle and western Oklahoma and Kansas, leading to widespread improvements to ongoing drought in the western Great Plains.
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