An upper trough will continue to move from the Pacific Northwest to the Upper Midwest. During its evolution, a series of disturbances aloft will work their way across the Intermountain West and into the Northern Plains and Upper Midwest. These impulses will help produce an extensive region of precipitation. Enough cold air aloft is available to produce snow at some of the highest elevations.
Ahead of the upper trough along the surface front, low-level moisture will be available to trigger numerous showers and thunderstorms over the Northern and Central Plains and into the Upper Midwest.
Hot and dry conditions will continue across the Desert Southwest and Four Corners Region.
An upper trough along the East Coast will finally begin to slowly shift north and east.
Daytime heating will continue to trigger thunderstorms over the region. Wet weather will continue over southern Florida.
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