2,076 first-hand accounts of flood events in Louisiana, ranked by impact. Each is a NOAA-written narrative of the moment.
A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma.
Read the full account →A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma.
Read the full account →A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma.
Read the full account →A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma.
Read the full account →A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma.
Read the full account →A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma.
Read the full account →A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma.
Read the full account →A closed upper low emerged out of the Rockies and into the Central Plains during the afternoon and evening hours of March 21st, with the attendant upper trough swinging east through Central Texas and Oklahoma.
Read the full account →A weak upper trough drifted south into East Texas and North Louisiana on August 10th, and provided enough large scale forcing for scattered showers and thunderstorms during much of the day across portions of North Louisiana.
Read the full account →A weak frontal boundary and associated surface low pressure remained stationary across North-central Louisiana on August 24th. Precipitable water values were on the order of two inches along and south of this boundary.
Read the full account →A weak frontal boundary and associated surface low pressure remained stationary across North-central Louisiana on August 24th. Precipitable water values were on the order of two inches along and south of this boundary.
Read the full account →A weak frontal boundary and associated surface low pressure remained stationary across North-central Louisiana on August 24th. Precipitable water values were on the order of two inches along and south of this boundary.
Read the full account →An upper level ridge was centered north and west of the region. That put the local area on the outer periphery of the ridge. Atmospheric moisture levels were very high, with a precipitable water value of 2.4 inches.
Read the full account →A meso-scale convective system (MCS) developed out of afternoon thunderstorms initiated along a frontal boundary in northern Alabama and Georgia on the 21st.
Read the full account →A meso-scale convective system (MCS) developed out of afternoon thunderstorms initiated along a frontal boundary in northern Alabama and Georgia on the 21st.
Read the full account →A meso-scale convective system (MCS) developed out of afternoon thunderstorms initiated along a frontal boundary in northern Alabama and Georgia on the 21st.
Read the full account →A meso-scale convective system (MCS) developed out of afternoon thunderstorms initiated along a frontal boundary in northern Alabama and Georgia on the 21st.
Read the full account →A meso-scale convective system (MCS) developed out of afternoon thunderstorms initiated along a frontal boundary in northern Alabama and Georgia on the 21st.
Read the full account →An upper level ridge was centered east of the area and another to the west. That put the local area in a region of weakness between them which is an area conducive for higher rain chances.
Read the full account →An upper level ridge was centered east of the area and another to the west. That put the local area in a region of weakness between them which is an area conducive for higher rain chances.
Read the full account →A cold front that was moving south across Mississippi and Louisiana on 6/9 moved across portions of the the local coastal waters. Sufficient instability was still in place from the previous afternoon to support severe thunderstorms along the boundary.
Read the full account →A cold front that was moving south across Mississippi and Louisiana on 6/9 moved across portions of the the local coastal waters. Sufficient instability was still in place from the previous afternoon to support severe thunderstorms along the boundary.
Read the full account →A cold front that was moving south across Mississippi and Louisiana on 6/9 moved across portions of the the local coastal waters. Sufficient instability was still in place from the previous afternoon to support severe thunderstorms along the boundary.
Read the full account →A cold front that was moving south across Mississippi and Louisiana on 6/9 moved across portions of the the local coastal waters. Sufficient instability was still in place from the previous afternoon to support severe thunderstorms along the boundary.
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