Flood in Bland County, Virginia

Several streams were out of banks and roads covered by flood waters.

A deep upper-level trough moved slowly across the central and eastern U.S. drawing abundant moisture northward. At the same time, a complex frontal boundary with several waves of low pressure brought repeated rounds of heavy rainfall to the region. Rainfall totals for the 72-hour period ending at 700 AM on February 7th ranged from 2 to 6 inches with isolated higher amounts mainly along the Blue Ridge Mountains, but most of the rain fell within a 48-hour period. Numerous NWS Cooperative stations recorded all time one-day February rainfall amounts ending on the morning of February 6th and/or the 7th, and numerous two-day February records were also set. Some flash flooding occurred early in the the event as higher rates of rainfall were embedded within the overall rain pattern. Numerous rivers and streams flooded, some reaching crests mainly in the 5- to 10-year flood recurrence interval and many roads were flooded. A state of emergency was declared by the Virginia Governor for several counties in southwest Virginia due to the flooding, including Tazewell and Smyth counties. Flooding was most severe along the Clinch River and tributaries in Richlands, VA where a Flash Flood Emergency was issued in consultation with local officials.