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Atmospheric Conditions that Led to the Roma, Texas Floods of August 2008
Handout (707.7 kB)
Through the period, a series of upper level disturbances moved across northern Mexico and the southwest United States. As each disturbance approached South Texas, a low level jet developed. Each jet likely transported very moist air across the higher terrain of the Rio Grande Plains toward the eastern slopes of the Sierra Madre Oriental mountains. The entire border region from Del Rio to McAllen, Texas, received heavy rainfall. In particular, extreme southern Zapata and southwestern Starr County, along the Rio Grande, experienced torrential rain-producing thunderstorms on five days.
The combination of synoptic and mesoscale features which produced this memorable flood will be discussed. Results from the analysis will help forecasters better predict the potential for localized significant flooding prior to future events in this portion of Deep South Texas.