2,771 first-hand accounts of flood events in Virginia, ranked by impact. Each is a NOAA-written narrative of the moment.
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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →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.
Read the full account →Southwest winds aloft were responsible for carrying deep tropical moisture across the Piedmont during the morning of the 21st, while northeasterly flow near the surface was in place due to high pressure wedged against the eastern face of the Appalachians.
Read the full account →One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.
Read the full account →One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.
Read the full account →One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.
Read the full account →One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.
Read the full account →One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.
Read the full account →Tropical Storm Isaias moved up the east coast, passing through southern Maryland on the morning of Tuesday, August 4th, 2020, spawning several tornadoes as well as flooding rain and tropical storm force winds.
Read the full account →One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.
Read the full account →One of the most significant flooding events in years occurred during November 11th and 12th, given both the amounts of rainfall and the footprint where flooding occurred.
Read the full account →