2,551 first-hand accounts of flood events in West Virginia, ranked by impact. Each is a NOAA-written narrative of the moment.
Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).
Read the full account →A stationary front located near West Virginia on the morning of February 16th acted as a link between two low pressure systems streaming north and south of the area.
Read the full account →A stationary front located near West Virginia on the morning of February 16th acted as a link between two low pressure systems streaming north and south of the area.
Read the full account →A stationary front located near West Virginia on the morning of February 16th acted as a link between two low pressure systems streaming north and south of the area.
Read the full account →A stationary front located near West Virginia on the morning of February 16th acted as a link between two low pressure systems streaming north and south of the area.
Read the full account →Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).
Read the full account →Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).
Read the full account →A stationary front located near West Virginia on the morning of February 16th acted as a link between two low pressure systems streaming north and south of the area.
Read the full account →A stationary front located near West Virginia on the morning of February 16th acted as a link between two low pressure systems streaming north and south of the area.
Read the full account →A stationary front located near West Virginia on the morning of February 16th acted as a link between two low pressure systems streaming north and south of the area.
Read the full account →Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).
Read the full account →Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).
Read the full account →Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).
Read the full account →Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).
Read the full account →Prolonged rainfall over a 24- to 25-hour period ended around 8 AM EST on February 17th, which resulted in localized minor river flooding across portions of southeast West Virginia (SEWV).
Read the full account →Showers and strong to severe thunderstorms sprouted in the afternoon and evening of June 3rd as a backdoor cold front approached and then pushed across the area.
Read the full account →In the midst of hot and muggy conditions ruling the roost over the Central Appalachians, diurnally driven showers and thunderstorms thrived near the end of July.
Read the full account →A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region.
Read the full account →A deep, closed upper level low pressure system was observed over central Alabama on the morning of May 28th. The east winds around this low, allowed deep sub-tropical moisture from the Atlantic to move into lower Mid-Atlantic region.
Read the full account →Ahead of a large cluster of showers and thunderstorms, new storms formed over western Kanawha County during the evening hours. These storms drifted north during the night, producing over 2 inches of rain in less than 3 hours.
Read the full account →Several rounds of showers and thunderstorms were along and south of a cold front. Areas of Fayette and Raleigh Counties were just recovering from the floods on the 8th, when renewed flooding hit.
Read the full account →Several rounds of showers and thunderstorms were along and south of a cold front. Areas of Fayette and Raleigh Counties were just recovering from the floods on the 8th, when renewed flooding hit.
Read the full account →An upper level trough, centered over the Ohio valley on the Sept 6th absorbed the remnants of Tropical Storm Lee allowing for deep moisture to slowly progress northward through the Mid-Atlantic states.
Read the full account →Convection formed during Labor Day afternoon. The air was warm and humid. A cold front was located over central Ohio. The prefrontal convection was in several small clusters, not a solid line.||One batch of storms and showers became oriented west to east along the flow during…
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