Catastrophic Flash Flooding in Texas Hill Country

7/16/26 Update @ 11am (See earlier report below the update.) – Widespread catastrophic flooding is occurring on the:

  • Pedernales River
  • Frio River
  • Guadalupe River
  • Nueces River 
  • Leona River
  • Sabinal River

Flash Flood Emergencies have been announced for: 

  • Guadalupe River (Hunt to Bergheim)
  • Pedernales River (Fredericksburg to Johnson City)
  • Frio River (Leakey to Concan)
  • All Uvalde County
  • All Central and eastern Kerr County
Guadalupe River: 

An initial catastrophic flood wave is passing Comfort.

The river at Comfort crested 2 feet above July 2025 levels.

Jeff Lindner, Harris County Meteorologist

This flood wave is now moving into western Kendall County.

A second floodwave of 15-20 feet has been generated on the south Fork upstream of Hunt TX and is moving into Hunt. It will impact Ingram and Kerrville in a secondary rise on the river similar to levels experienced this morning.

This remains a life-threatening situation along the river from upstream of Hunt to downstream into Kendall County. Catastrophic damage has occurred and is occurring along the river. Numerous swift water and air asset rescues from trees and rooftops are ongoing.   

Frio River: 

Major to catastrophic flooding is ongoing from Leakey to Concan. River is approaching record levels at Leakey upstream of Concan. Disastrous flooding with up to 10 feet of flow inundating all camp grounds from Rio Frio into Concan and downstream toward Uvalde. Much of Garner State Park is flooded. All low water crossing are flooded and impassable.

Pedernales River: 

Major to catastrophic flooding from the headwaters into Fredericksburg downstream to Johnson City. Evacuations underway along the river. Considerable damage will occur near LBJ ranch.

From 8am Earlier Today

7/16/26 @ 9am – Jeff Lindner, Harris County’s meteorologist, reports that there is ongoing catastrophic flash flooding this morning across the Texas Hill Country.

Kerr County officials have declared a flash flood emergency for the Guadalupe River from Ingram to Comfort.

Ditto for Uvalde County where there is catastrophic flooding likely along the Frio, Leona, Sabinal, and Nueces Rivers.

8-10 Inches of Rainfall Overnight

Rainfall since midnight of 8-10 inches over Hunt and Ingram has resulted in a 20-30 foot rise in the Guadalupe River downstream of Hunt. Catastrophic life-threatening flooding is occurring. Numerous evacuations of camp grounds are in progress along the river and Johnson Creek.

Water levels in Ingram rose 25 feet in a few hours and peaked five feet below July 2025 levels. A destructive flood wave is moving down the Guadalupe River into Kerrville and toward Centerpoint and Comfort. The river has risen 32 ft in just four hours at Centerpoint, Texas, and is likely to reach July 2025 levels at this location.

The river at Comfort rose 16 feet in just 30 minutes this morning.

Rainfall of 15-30 inches has occurred over portions of Uvalde, Medina, and Real Counties in the last 48 hours.

Catastrophic flooding is ongoing across Uvalde County along the Frio, Leona, Sabinal, and Nueces Rivers.

The forecast crest on the Frio River at Concan will result in damaging flooding to camps along the river below Rio Frio into Concan. Rises along the Leona River will approach or equal levels seen yesterday resulting in widespread flooding in the City of Uvalde.  

Significant downstream moving flood waves are being generated on several of these rivers. They will continue into the weekend.


Defining Characteristics of Flash Flooding

The defining characteristic of flash flooding is speed. Unlike most other forms of flooding, flash floods develop rapidly — typically within 6 hours of the rainfall event, and often within 1 to 3 hours. That rapid onset leaves little time for warnings or evacuation.

Here’s how flash flooding differs from other common types of flooding, according to ChatGPT:

Flood TypeTypical OnsetPrimary CauseTypical DurationGreatest Hazard
Flash floodingMinutes to <6 hoursIntense rainfall, dam or levee failureHoursSudden rise, high velocity
River floodingDays to weeksProlonged rainfall, snowmeltDays to weeksLarge geographic extent
Coastal floodingHours to daysStorm surge, high tidesHours to daysSaltwater inundation
Urban floodingMinutes to hoursRainfall exceeds drainage capacityHoursStreets and buildings inundated
Pluvial (surface water) floodingHoursHeavy rainfall independent of riversHours to a dayPonding in low areas

What Makes a Flash Flood “Flash”?

Several conditions combine:

  • Very intense rainfall (for example, several inches per hour)
  • Small drainage basins that respond quickly
  • Steep terrain where water accelerates downhill
  • Impervious surfaces such as pavement and rooftops
  • Limited storage in soils, wetlands, or detention basins

The hydrograph of a flash flood has a very steep rising limb, meaning stream levels can increase several feet in minutes.

For More Information

The Hill Country Flooding has attracted the attention of media nationwide:

Posted by Bob Rehak on 7/16/2026 @ 9am

3243 Days since Hurricane Harvey

TWDB Publishing Nature-Based Solutions Guide

7/10/2026 – The Texas Water Development Board (TWDB) has published a Draft Nature-Based Solutions (NBS) Guide for Flood Resilience in Texas. It’s one of a number of documents in development for the next iteration of the State’s Flood Plan. And they are seeking stakeholder feedback.

The 314-page document is a 130 meg download, so don’t try to view it on your phone. But it is well researched, written, and illustrated. It seeks to equip local officials, engineers, community planners, and flood-related professionals with the knowledge they need to go beyond gray. Community activists may also find the Guide helpful in initiating discussions with those groups and pointing out opportunities.

Practical Step-By-Step Guide

The draft guide presents a clear framework for planning, implementing, and maintaining NBS as part of comprehensive flood resilience strategies. It includes solutions at both the watershed-scale and neighborhood scale. It is a practical step-by-step framework for:

  • Initiating
  • Planning
  • Implementing projects.

The guide contains 13 chapters in those three broad categories:

  • Laying the groundwork for NBS
  • Introducing NBS for flood resilience
  • Embracing guiding principles for NBS
  • Assessing ordinances incentives and Regulations
  • Establishing funding strategies
  • Integrating NBS into planning processes
  • Understanding flood risk and identifying flood-risk opportunities
  • Evaluating NBS feasibility and alternatives
  • Designing and building NBS
  • Applying watershed NBS design and construction considerations
  • Applying neighborhood NBS design and construction considerations
  • Applying coastal NBS design and construction considerations
  • Maintaining and adaptively managing NBS

The concepts are not theoretical. They are being successfully implemented across Texas – from floodplain buyouts to stormwater parks, regional watershed planning, and living shoreline projects. And the attractive illustrations from around the state encourage readers to dig in and explore.

Photo of Fort Work Stormwater Park courtesy of Freese and Nichols, Inc.

From Planning to Identifying Opportunities and Construction

As I was browsing through it, two chapters forced me to dig down immediately: Chapter 6 on Planning and Chapter 7 on understanding flood risk and identifying NBS opportunities.

A table in Chapter 6 mentioned examples of needs in the San Jacinto watershed including “Preserve and restore … river floodplains to improve … natural storage, and resilience to compound flooding.”

It was exactly what I have been advocating for the Scarborough property and San Jacinto West Fork sand-mining gauntlet. Then the chapter discussed ways to identify and reach out to stakeholder groups.

Chapter 7 includes sections on determining flood risks and identifying flood risk hot spots. It also included an “Opportunity Matrix Tool” to help convert “Needs” to “Solutions.”

Subsequent chapters include the nuts and bolts of how to do that. The work is broken up into quick, readable sections with charts, tables, graphs, photos and illustrations that help readers grasp concepts at a glance.

How Green and Gray Can Work Together

All in all, for those threatened by flooding and those who represent them, this guide presents a step-by-step framework for implementing nature-based solutions, either alone or in combination with other flood mitigation projects. The emphasis is on how green and gray solutions can work together. And that’s refreshing.

Click here to download the document. Warning 130 Megs.

Posted by Bob Rehak on 7/10/26

3237 Days since Hurricane Harvey

The Complexity of Accurately Estimating Current Flood Risk

7/9/2026 – A young couple that is considering buying a home in my neighborhood asked me a simple question yesterday? “What is the current flood risk?” The home they were considering flooded during Hurricane Harvey. But that was an extreme event. And they wondered whether mitigation activities since then would prevent it from flooding again.

I tried to explain the various mitigation efforts since then and the current status of each. However, I quickly realized that the scale, complexity, relative impact and timing of the efforts make the task of estimating “current” flood risk virtually impossible. They are all at different stages. And few are complete.

Kingwood Flooding
Flooding neighborhood near Kingwood Country Club in May 2024, a less-than-Harvey event, but which still saw one of the largest releases ever from Lake Conroe.

What Goes into Calculating Flood Risk?

Flood risk is not static. Estimates change constantly. Predicting what will fall from the sky and where once every 100 or 500 years is only part of the battle. To name just a few things, we also need to understand:

  • How the landscape is changing
  • Where people are building
  • How they are building, i.e., elevated structures vs. slab on grade
  • What they are doing to offset increased runoff
  • Soil types and rates of infiltration
  • Changes in land-use patterns, i.e., forestry vs. retail development
  • Reservoir operations
  • Sediment accumulations, such as deltas, that can reduce channel conveyance
  • Bridges that can create backwater effects
  • Subsidence that can alter channel gradients
  • Flood-mitigation efforts and their impacts
  • Timing effects, such as the “stacking effect” at confluences, can erode margins of safety
  • Changes in regulations in and across different parts of a watershed

Impacts of Uncertainty and Misunderstanding on Estimates

Understanding the impact of those factors on uncertainty may require a graduate degree in statistics. Every flood risk estimate contains uncertainty arising from:

  • Rainfall estimates
  • Future land development
  • Climate variability
  • Hydraulic model assumptions
  • Terrain (LiDAR) accuracy
  • Roughness coefficients
  • Reservoir operations
  • Future sedimentation
  • Infrastructure changes

Then, layer on semantic confusion. To most people, a “100-year flood” sounds like one that happens once a century. But it actually has a 1% annual chance of occurring in any given year. Theoretically, you could have back-to-back-to-back 100-year floods, as we did in 2015, 2016 and 2017.

A 1% chance is no guarantee that a flood of that magnitude will only occur once every 100 years.

In fact, a 1% annual chance flood has a 26% chance (about 1 in 4) of occurring during the life of a 30-year mortgage. And that assumes nothing changes in the watershed. This often surprises people. Here’s how to calculate it.

And here’s how the probabilities break down for various return periods.

Annual ChanceReturn PeriodChance Over 30 Years
10%10-year flood95.8%
4%25-year flood70.6%
2%50-year flood45.5%
1%100-year flood26.0%
0.2%500-year flood5.8%

Interaction of Factors Can Amplify Risk

Many of the issues above interact in ways that can amplify risk. For example:

  • Rapid urbanization increases impervious cover and runoff
  • Sedimentation and subsidence reduce channel conveyance
  • Reservoir operations influence the timing and magnitude of downstream flows
  • Political fragmentation can make watershed-wide coordination more difficult.

In combination, these factors mean that flood risk is not static. It evolves as the watershed, the built environment, regulations, and flood mitigation activities change…at different rates…across dozens of jurisdictions.

Complexity, Timing Make Current Risk Virtually Unknowable

The scale, complexity, interaction and timing of these factors makes accurate assessment of current flood risk virtually impossible eight years after data for the new flood maps was collected in 2018.

Since then, Montgomery County has been one of the fastest growing counties in America. Yet it didn’t update its floodplain regulations until 2025. And there’s no way to quantify how vigorously it has enforced its regulations.

During that time, Harris County and City of Houston have engaged in many mitigation activities, i.e., dredging. But since the dredging, sediment from sand mines and natural erosion has built back in somewhat. But how much?

Confluence of West Fork and Spring Creek.
Confluence of Spring Creek and West Fork showing sediment pollution coming from West Fork and its sand mines.

There are no current surveys of water depth that I know of.

Advice for Homebuyers

Given all the uncertainty, experts recommend that homebuyers:

  • Look beyond FEMA flood maps. They are valuable, but have limitations and may be outdated.
  • Research the property’s actual flood history. Don’t rely solely on the seller’s disclosure. Talk with neighbors—they often know the area’s history better than anyone.
  • Study the topography, local drainage, storm sewers, elevation, nearby creeks, and ditches
  • Consider how the area is changing. Runoff can increase over time in a rapidly urbanizing watershed
  • Don’t assume “never flooded” means “never will.” 
  • Understand the residual risk behind flood-control infrastructure. Levees, reservoirs, detention basins, and drainage projects reduce risk in smaller floods, but increase it in larger ones by creating a false sense of security that encourages people to build in risky areas
  • Evaluate flood insurance – even if it’s not required. 
  • Think long term. Ask how conditions could change in 10, 20 or 30 years
  • Be cautious with unusually attractive prices. Sometimes a lower purchase price reflects higher flood risk. That doesn’t automatically make it a bad purchase, but you should weigh the discount against higher insurance costs, potential repair costs, and resale challenges.
  • Ask yourself “If this home flooded, could I recover financially and emotionally?” If the answer is no, that should weigh heavily in your decision to buy the property.

Posted by Bob Rehak on 7/9/2026

3236 Days since Hurricane Harvey