4,808 first-hand accounts of flood events in Texas, ranked by impact. Each is a NOAA-written narrative of the moment.
An upper level shortwave trough moved around the longwave low over the Four Corners region. This upper distubance interacted with a surface boundary moving northward as a warm front from South Texas into a very moist airmass.
Read the full account →An upper level shortwave trough moved around the longwave low over the Four Corners region. This upper distubance interacted with a surface boundary moving northward as a warm front from South Texas into a very moist airmass.
Read the full account →Very high moisture was left over South Texas on the 17th as the remnants of Tropical Storm Bill moved northward into north-central Texas. Numerous showers and thunderstorms produced flash flooding in the morning across the Victoria Crossroads and in the afternoon over the…
Read the full account →Very high moisture was left over South Texas on the 17th as the remnants of Tropical Storm Bill moved northward into north-central Texas. Numerous showers and thunderstorms produced flash flooding in the morning across the Victoria Crossroads and in the afternoon over the…
Read the full account →Tropical storm Bill moved onshore over Matagorda Island on the morning of June 16th. The center of Bill moved through Lavaca, Fayette, and Lee Counties on the 17th. The strongest recorded wind gust was 47 mph near Schulenburg in Fayette County.
Read the full account →Tropical storm Bill moved onshore over Matagorda Island on the morning of June 16th. The center of Bill moved through Lavaca, Fayette, and Lee Counties on the 17th. The strongest recorded wind gust was 47 mph near Schulenburg in Fayette County.
Read the full account →A frontal boundary stalled north of the South Texas region during the morning hours on May 11th. Scattered thunderstorms developed in the afternoon over the Brush Country. A supercell thunderstorm was nearly stationary over southern Duval County for several hours.
Read the full account →An upper level shortwave trough moved around the longwave low over the Four Corners region. This upper distubance interacted with a surface boundary moving northward as a warm front from South Texas into a very moist airmass.
Read the full account →An upper level shortwave trough moved around the longwave low over the Four Corners region. This upper distubance interacted with a surface boundary moving northward as a warm front from South Texas into a very moist airmass.
Read the full account →An upper level shortwave trough moved around the longwave low over the Four Corners region. This upper distubance interacted with a surface boundary moving northward as a warm front from South Texas into a very moist airmass.
Read the full account →A frontal boundary moved out of the Hill Country as the upper level disturbance moved into northwest Texas and western Oklahoma early on the 14th.
Read the full account →A frontal boundary stalled north of the South Texas region during the morning hours on May 11th. Scattered thunderstorms developed in the afternoon over the Brush Country. A supercell thunderstorm was nearly stationary over southern Duval County for several hours.
Read the full account →A frontal boundary stalled north of the South Texas region during the morning hours on May 11th. Scattered thunderstorms developed in the afternoon over the Brush Country. A supercell thunderstorm was nearly stationary over southern Duval County for several hours.
Read the full account →A frontal boundary stalled north of the South Texas region during the morning hours on May 11th. Scattered thunderstorms developed in the afternoon over the Brush Country. A supercell thunderstorm was nearly stationary over southern Duval County for several hours.
Read the full account →An upper level shortwave trough moved around the longwave low over the Four Corners region. This upper distubance interacted with a surface boundary moving northward as a warm front from South Texas into a very moist airmass.
Read the full account →An upper level shortwave trough moved around the longwave low over the Four Corners region. This upper distubance interacted with a surface boundary moving northward as a warm front from South Texas into a very moist airmass.
Read the full account →An upper level shortwave trough moved around the longwave low over the Four Corners region. This upper distubance interacted with a surface boundary moving northward as a warm front from South Texas into a very moist airmass.
Read the full account →A frontal boundary stalled north of the South Texas region during the morning hours on May 11th. Scattered thunderstorms developed in the afternoon over the Brush Country. A supercell thunderstorm was nearly stationary over southern Duval County for several hours.
Read the full account →A frontal boundary stalled north of the South Texas region during the morning hours on May 11th. Scattered thunderstorms developed in the afternoon over the Brush Country. A supercell thunderstorm was nearly stationary over southern Duval County for several hours.
Read the full account →Tropical storm Bill moved onshore over Matagorda Island on the morning of June 16th. The center of Bill moved through Lavaca, Fayette, and Lee Counties on the 17th. The strongest recorded wind gust was 47 mph near Schulenburg in Fayette County.
Read the full account →Tropical storm Bill moved onshore over Matagorda Island on the morning of June 16th. The center of Bill moved through Lavaca, Fayette, and Lee Counties on the 17th. The strongest recorded wind gust was 47 mph near Schulenburg in Fayette County.
Read the full account →Tropical storm Bill moved onshore over Matagorda Island on the morning of June 16th. The center of Bill moved through Lavaca, Fayette, and Lee Counties on the 17th. The strongest recorded wind gust was 47 mph near Schulenburg in Fayette County.
Read the full account →An upper level shortwave trough moved around the longwave low over the Four Corners region. This upper distubance interacted with a surface boundary moving northward as a warm front from South Texas into a very moist airmass.
Read the full account →A frontal boundary moved out of the Hill Country as the upper level disturbance moved into northwest Texas and western Oklahoma early on the 14th.
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