2,548 first-hand accounts of flood events in North Carolina, ranked by impact. Each is a NOAA-written narrative of the moment.
A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County.
Read the full account →A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County.
Read the full account →A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County.
Read the full account →A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County.
Read the full account →A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County.
Read the full account →A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County.
Read the full account →A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County.
Read the full account →A meso-scale boundary along the North Carolina-Virginia state line sparked a complex of slow moving convection that produced 4 to 5 inches of rain and isolated flash flooding across Person County.
Read the full account →Heavy rain showers and thunderstorms developed over central NC in association with a series of disturbances moving through the long wave trough aloft. Deep moist advection and unidirectional flow through the atmosphere resulted in training of heavy rain and thunderstorms.
Read the full account →Heavy rain showers and thunderstorms developed over central NC in association with a series of disturbances moving through the long wave trough aloft. Deep moist advection and unidirectional flow through the atmosphere resulted in training of heavy rain and thunderstorms.
Read the full account →Heavy rain showers and thunderstorms developed over central NC in association with a series of disturbances moving through the long wave trough aloft. Deep moist advection and unidirectional flow through the atmosphere resulted in training of heavy rain and thunderstorms.
Read the full account →Deep Gulf of Mexico moisture channeling between an amplifying trough over the mid-lower MS Valley and the western Atlantic ridge led to precipitable waters increasing to to over 2.0 over the area.
Read the full account →An upper ridge off the east coast and an upper low over the central U.S. combined to bring enhanced moisture into the region. Weak low pressure along a frontal boundary draped near the Virginia-North Carolina border provided additional convergence and lift to produce widespread…
Read the full account →Deep Gulf of Mexico moisture channeling between an amplifying trough over the mid-lower MS Valley and the western Atlantic ridge led to precipitable waters increasing to to over 2.0 over the area.
Read the full account →Deep Gulf of Mexico moisture channeling between an amplifying trough over the mid-lower MS Valley and the western Atlantic ridge led to precipitable waters increasing to to over 2.0 over the area.
Read the full account →Deep Gulf of Mexico moisture channeling between an amplifying trough over the mid-lower MS Valley and the western Atlantic ridge led to precipitable waters increasing to to over 2.0 over the area.
Read the full account →An upper ridge off the east coast and an upper low over the central U.S. combined to bring enhanced moisture into the region. Weak low pressure along a frontal boundary draped near the Virginia-North Carolina border provided additional convergence and lift to produce widespread…
Read the full account →A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th.
Read the full account →A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th.
Read the full account →A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th.
Read the full account →A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th.
Read the full account →A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th.
Read the full account →A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th.
Read the full account →A ridge of high pressure over eastern North America stalled Florence's forward motion a few miles off the southeast North Carolina coast on September 13th.
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