National Weather Service United States Department of Commerce

Monday Night Madness:  "Great June Flood II" in 2019 Strikes Willacy, Eastern Hidalgo, and Northwest Cameron on June 24th

It was déjà vu all over again.

Just 367 days after the last of the Great June Flood of 2018 had left its memorable mark on nearly all of the populated Rio Grande Valley, a confluence of atmospheric events came together during the late afternoon and evening of June 24th, 2019, to produce another memorable - and unfortunate - situation for parts of the Rio Grande Valley. This time, the impacted area was smaller and less populated but the results the same. For most of Willacy County's population, the western third of Cameron, and a corner of eastern Hidalgo, the following occurred:

  • Over a foot of rain fell in about six hours, including a peak total of more than 15 inches near Santa Rosa (Cameron/Hidalgo line)
  • Hundreds of streets flooded, including 30 Texas-managed highways.
  • 1,188 homes were considered "destroyed" or incurring "major" damage requiring significant repairs. An additional 182 homes sustained "minor" damage or were mildly affected (as of July 10)
  • Individual Assistance (IA) costs were estimated at $27.6 million. Public Assistance (PA) costs had not yet been factored in (July, 2019)
  • Total damage is likely to range from $50 to $100 million or more when all estimates have been received. Final estimated may not be known until late 2019.
  • More than 100 persons were evacuated to safe high ground from dozens of homes threatened by 2 or more feet of water in several locations in each county
  • At least 45,000 private and public utility power customers were without power at the peak of the storm
  • Estimated 65 to 75 mph winds caused at least five poorly built mobile homes to be rolled or demolished in eastern Hidalgo County
  • Lightning struck a wind turbine and set it ablaze in Willacy County
New daily rainfall records were set at most available Rio Grande Valley climate recording locations. These included:
  • Raymondville, with 9.7 inches* (prior:  1.83 inches in 1922; new June daily record - prior: 6.23 inches on 6/21/1993)
  • Weslaco, with 6.95 inches* (prior:  3.72 inches in 1951)
  • Harlingen, with 6.29 inches* (prior:  2.23 in 1926; new June daily record - prior:  5.89 inches on 6/20 2018)
  • McAllen, with 3.30 inches (prior:  1.83 inches in 1973)
  • Edinburg, with 2.49 inches* (prior:  1.36 inches in 2014)
  • Brownsville, with 2.06 inches (prior:  2 inches in 1920)
*Based on 7 AM to 7 AM records

These single day rainfall totals, except for Brownsville and Edinburg, were above the monthly averages for June. For Harlingen, and Weslaco, these values were around three times the monthly average, and more than four times the monthly average for Raymondville.

Cities and towns with the most impact included:

  • Raymondville (Willacy Co) - The entire north half of the city's streets were flooded, with dozens if not more than 100 homes and business taking on inches to feet of water
  • Sebastian (Willacy Co) - All neighborhood streets were flooded due to rainfall and drainage issues through the 25th and beyond
  • Harlingen/Primera (Cameron Co) - Frontage roads, businesses along them, and neighborhoods - all north of Interstate 2 - had multiple flood issues due to rainfall and overwhelmed drainage systems
  • La Feria through Mercedes (Cameron/Hidalgo Line) - Same situation as portions of northwest Harlingen. This was the primary area of overlapping impacts similar to the June 2018 event, just one year later.
  • Elsa through Monte Alto colonias, occurred (see Wind Damage tab for more). At least five residences were demolished, one rusting grain silo tower collapsed, and dozens of trees were uprooted and numerous tree limbs blown down. Flooding rains and poor drainage left at least 4 feet of water in at least one neighborhood, requiring evacuations.

In addition to the neighborhood flooding, the location and intensity of the rainfall poured into Arroyo Colorado, with quite a bit of outflow into the Rio Grande as well.

  • The Arroyo Colorado crested at 22.67 feet, the highest level since June 2018 and the fourth highest on record. It was the second time in two years that only runoff from rainfall caused the rises. The high water flooded parks and other activities inside the levee.
  • The Rio Grande near San Benito was forecast to crest near 44 feet and near Brownsville, up to 14 feet, as of this writing.

Different Situation, Similar Result

Unlike the Great June Flood of 2018, the atmospheric setup couldn't have been any more different. This time, the situation - one that had been a persistent feature since April - was setup by yet another energy wave that moved through north central and east Texas, and spawned another round of severe weather (wind/hail) on Sunday, June 23rd. This was the initial feature that set the table to trigger the crazy...and scary...events of June 24th:

  • Ingredient 1: A thunderstorm "system" in southeast Texas. This system, moving to the right of the mean atmospheric flow, rolled through southeast Texas, including Houston/Galveston, on its way to the Gulf by daybreak Monday. It would propagate on its own momentum into the western Gulf, still hugging the Texas coast, with a slow but steady movement toward the Coastal Bend.
  • Ingredient 2: Southeast to east "inflow" and daytime heating = Supercell. Incredibly persistent heat and humidity across south Texas combined with colliding southeasterly flow with the northerly winds along the boundary began new thunderstorm develop near Kingsville a little after noon on the 24th. That cell would continue to feed on moisture inflow and the turning winds to produce a high-precipitation supercell thunderstorm in Kenedy County.
  • Ingredient 3: Multiple colliding boundaries and supercell slowdown. Between 5 and 6 PM, as the supercell storm was still producing strong to destructive winds and pockets of large hail, outflow boundaries propagating west and southwest fed on the near record heat and oppressive humidity to produce expansive clusters of storms that spread quickly into Hidalgo and Starr County. Other boundaries from the old main line in the Gulf, and new storms in northern Mexico, fed the beast. At the same time, the entire system slowed before reaching the Rio Grande as evening approached and the earlier boundaries ran out of momentum.
  • Ingredient 4: Coalescence and Upper Level Assistance. The development of mesoscale high and low pressure couplets along with favorable upper level winds allowed for a broad circulation to form, centered near the triple county lines of Hidalgo, Willacy, and Cameron, by mid evening of the 24th. Pulsing storms within the circulation maintained intense rainfall, up to the rate of 3 inches per hour, from 8 PM to midnight - which completed the transition from a mixed severe weather and flood event to a predominant flood event that spread into all of western Cameron County while continuing over western Willacy and far eastern Hidalgo County.

Additional details will be added to this report into July as more data are received from emergency management and other partners following damage assessments.

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