2,894 first-hand accounts of flood events in Missouri, ranked by impact. Each is a NOAA-written narrative of the moment.
This is a continuation of the heavy rainfall event that started May 31. A mesoscale convective vortex continued to produce heavy rainfall across portions of southern Missouri where localized amounts over 6 inches occurred.
Read the full account →This is a continuation of the heavy rainfall event that started May 31. A mesoscale convective vortex continued to produce heavy rainfall across portions of southern Missouri where localized amounts over 6 inches occurred.
Read the full account →This is a continuation of the heavy rainfall event that started May 31. A mesoscale convective vortex continued to produce heavy rainfall across portions of southern Missouri where localized amounts over 6 inches occurred.
Read the full account →This is a continuation of the heavy rainfall event that started May 31. A mesoscale convective vortex continued to produce heavy rainfall across portions of southern Missouri where localized amounts over 6 inches occurred.
Read the full account →This is a continuation of the heavy rainfall event that started May 31. A mesoscale convective vortex continued to produce heavy rainfall across portions of southern Missouri where localized amounts over 6 inches occurred.
Read the full account →This is a continuation of the heavy rainfall event that started May 31. A mesoscale convective vortex continued to produce heavy rainfall across portions of southern Missouri where localized amounts over 6 inches occurred.
Read the full account →This is a continuation of the heavy rainfall event that started May 31. A mesoscale convective vortex continued to produce heavy rainfall across portions of southern Missouri where localized amounts over 6 inches occurred.
Read the full account →A low pressure system moved northeast out of the Southern Plains May 8th into the early morning hours of May 9th, 2009. A MCS developed in association with the low and tracked across Northeast Arkansas, the Missouri Bootheel and Northwest Tennessee.
Read the full account →The weather pattern began to quiet down after the historic spring river flooding. With high pressure generally in control of the weather, the first half of June was very warm and dry.
Read the full account →An outflow boundary developed and moved southward into southern Missouri before interacting with a low level jet to produce additional heavy rainfall and isolated wind damage during the overnight hours of the 3rd into the morning of the 4th.
Read the full account →A line of showers and thunderstorms approached the city of Springfield from the west. This line of storms produced three to six inches of rain over the city causing flash flooding leading to numerous water rescues.
Read the full account →A line of showers and thunderstorms approached the city of Springfield from the west. This line of storms produced three to six inches of rain over the city causing flash flooding leading to numerous water rescues.
Read the full account →Several rounds of strong to severe storms developed from the evening of the 1st to the early morning of the 3rd as a surface low pressure system tracked from western Kansas southeastward into Red River Valley.
Read the full account →Several rounds of strong to severe storms developed from the evening of the 1st to the early morning of the 3rd as a surface low pressure system tracked from western Kansas southeastward into Red River Valley.
Read the full account →Several rounds of strong to severe storms developed from the evening of the 1st to the early morning of the 3rd as a surface low pressure system tracked from western Kansas southeastward into Red River Valley.
Read the full account →Several rounds of strong to severe storms developed from the evening of the 1st to the early morning of the 3rd as a surface low pressure system tracked from western Kansas southeastward into Red River Valley.
Read the full account →Several rounds of strong to severe storms developed from the evening of the 1st to the early morning of the 3rd as a surface low pressure system tracked from western Kansas southeastward into Red River Valley.
Read the full account →Several rounds of strong to severe storms developed from the evening of the 1st to the early morning of the 3rd as a surface low pressure system tracked from western Kansas southeastward into Red River Valley.
Read the full account →Several rounds of strong to severe storms developed from the evening of the 1st to the early morning of the 3rd as a surface low pressure system tracked from western Kansas southeastward into Red River Valley.
Read the full account →Several rounds of strong to severe storms developed from the evening of the 1st to the early morning of the 3rd as a surface low pressure system tracked from western Kansas southeastward into Red River Valley.
Read the full account →During the afternoon, a line of thunderstorms produced heavy rainfall. These storms occurred just south of a warm front under a very strong southwest low level flow, around 60 knots at 850 mb. An upper level disturbance over the Ozark Mountains contributed to the storms.
Read the full account →Two areas of storm activity affected the region during the morning hours. Storms that developed over western Kansas on the evening of the 23rd tracked eastward into southeast Kansas and western Missouri during the morning of the 24th.
Read the full account →A series of discrete thunderstorms, a few of which displayed supercell characteristics, moved east across southeast Missouri during the evening.
Read the full account →A series of discrete thunderstorms, a few of which displayed supercell characteristics, moved east across southeast Missouri during the evening.
Read the full account →