9/16/2026 – In my previous post, I summarized causes of flooding. I grouped 83 contributing factors into three main categories: nature, things humans do, and things humans fail to do. In my continuing effort to summarize years of research, today, I would like to summarize major categories of flood-mitigation solutions.
Major Categories of Flood-Mitigation Solutions
Flood mitigation is fundamentally about managing water better and reducing human vulnerability as development expands throughout watersheds. Below, I have grouped solutions into several major categories to make them easier to comprehend and remember. Each category lists multiple specific solutions within it that I have previously posted about.
1. Reduce runoff at the source
Keep rainfall from quickly becoming runoff. Preserve forests and natural areas. Limit unnecessary impervious cover with green alternatives, such as permeable pavement, rain gardens, bio-swales, green roofs, soil restoration, infiltration practices, and development standards that control post-development runoff.
While particularly useful for moderate storms, during extreme events, soils and small-scale storage can easily become saturated. So, view them as one layer of protection.
2. Preserve natural storage
This is almost always cheaper than trying to recreate storage after development.
Protect floodplains, wetlands, natural depressions, riparian corridors and other areas where water can temporarily spread without causing substantial damage.
The fundamental principle is:
Don’t eliminate storage you will later have to replace with expensive engineered storage.
3. Detain or retain excess runoff
Where development has already increased runoff, temporarily store the excess.
Solutions include detention basins, regional detention facilities, retention ponds, wetlands, underground storage and flood-control reservoirs. But don’t evaluate storage solely by acre-feet. Its location, outlet capacity and release timing also matter. A detention basin that releases water at the wrong time can contribute to downstream peaks.
4. Improve conveyance
Once water enters the drainage network, there must be enough capacity to move it safely.
Rustling Elms Bridge over Taylor Gully during peak of May 7, 2019, flood.
Moving water faster isn’t necessarily flood mitigation if the receiving system cannot handle it.
Improving conveyance upstream without considering downstream capacity can simply transfer the flood problem downstream.
5. Remove bottlenecks
The weakest link in a drainage system limits the entire system’s effectiveness.
A watershed may have ample channel capacity except for one undersized bridge, culvert, railroad crossing, utility crossing, sediment deposit or other constriction. This is especially important in an area, such as Houston, with flat terrain.
Sand deposited by Hurricane Harvey blocked San Jacinto West Fork by 90% according to Army Corps.
6. Manage sediment
Sediment management is especially relevant to the San Jacinto/Lake Houston system.
Possible mitigation measures include erosion prevention, construction-site BMP enforcement, stream-bank stabilization, better sand-mining practices, setbacks from channels, protection against pit capture, sediment traps where appropriate, dredging, and maintaining critical channel and tributary-mouth conveyance.
The objective: prevent excessive human-caused sedimentation from reducing critical conveyance or storage.
7. Manage flood peaks better
When water arrives affects flood peaks as much as how much arrives.
Potential solutions include coordinated reservoir operations, coordinated detention releases, strategically located regional detention, watershed-scale hydrologic modeling, real-time rainfall/stream monitoring, forecast-informed operations and—in some circumstances—pre-releases.
The goal: to avoid peaks from multiple tributaries, detention systems and reservoirs arriving at the same location at approximately the same time and stacking on each other.
8. Protect structures
Where development already exists in locations that have become hazardous, take steps to protect structures.
Examples include home elevation, floodproofing, floodwalls, levees, berms, gates, pumps, backflow prevention, elevated utilities and protection of critical facilities.
These measures generally reduce damage rather than eliminate flooding. But understand that a levee or floodwall, like the one at Kingwood High School, can reduce risk without making the protected area flood-proof.
9. Remove development from and/or stop developing in the highest-risk locations
Sometimes the most durable flood-control is simply to stop putting valuable things where water wants to go repeatedly.
Measures include voluntary buyouts, property acquisition, conversion of repetitive-loss areas to open space, preventing redevelopment of acquired properties, stricter floodway development restrictions, and avoiding new critical facilities in flood-prone areas.
Maintenance is one of the least glamorous and most important mitigation strategies.
Maintain channels, storm sewers, inlets, culverts, detention basins, pumps, gates and outfalls; remove debris and problematic sediment; repair erosion; inspect infrastructure; and preserve the designed storage and conveyance capacity.
A drainage system’s capacity should not be considered fixed at the capacity it had when constructed.
Without maintenance, design capacity deteriorates and flood risk increases.
11. Enforce the rules already on the books
New regulations accomplish little if existing ones aren’t enforced.
That includes floodplain/floodway restrictions, detention requirements, no-net-fill requirements, construction BMPs, stormwater permits, wetland requirements, mining permits, drainage easements and development conditions.
Flood infrastructure often lasts many decades. Designing only for today’s watershed can lock in future problems.
Planning should consider growth of impervious cover, upstream development, updated rainfall probabilities, subsidence, land-use change, downstream constraints and reasonably foreseeable changes in watershed hydrology.
This means building in generous safety margins. Development projects should do more than meet minimum requirements. They should still keep residents safe as the watershed develops.
13. Coordinate across the river basin
Floodwaters don’t recognize municipal or county boundaries. Effective mitigation therefore requires shared rainfall assumptions, compatible design standards, watershed-wide models, coordinated detention, reservoir operations, development assumptions, sediment management and capital planning.
It also requires a single accountable authority to “own” problems. Otherwise one jurisdiction’s successful drainage project can become another jurisdiction’s increased inflow.
14. Improve forecasting, warning and preparedness
These actions don’t prevent flooding. But they can dramatically reduce its consequences…as we learned in the Hill Country flooding at Camp Mystic.
Better rainfall forecasts, stream gauges, reservoir gauges, inundation forecasts, warning systems, evacuation planning, emergency communications and public education can save lives and property.
9/14/2026 – “Causes of flooding summarized” is part of my continuing effort to boil down more than 2 million words in 3100 posts since Hurricane Harvey into short summaries of key topics. I’ve seen the 83 causes of flooding listed below happen over and over again in different places in different combinations at different times. With the help of ChatGPT, I’ve organized them into three main groupings: Nature, What Humans Do, and What We Fail to Do.
The Three Large Groupings
1. NATURE — Conditions We Largely Cannot Control
These establish the underlying hydrologic and hydraulic setting.
Factor
Principal effect
Extreme rainfall intensity
Overwhelms infiltration and drainage capacity
Extreme rainfall duration
Produces large runoff volumes and sustained high flows
Tropical storms and hurricanes
Can produce both extreme rainfall and surge
Training/stalled thunderstorms
Repeatedly dumps rain over the same watershed
Antecedent rainfall
Saturated soils produce much greater runoff
Naturally low infiltration soils
Converts a larger percentage of rainfall to runoff
Flat terrain/low gradients
Slows drainage and increases backwater sensitivity
Watershed size and shape
Controls concentration and timing of runoff
Tributary geometry
Can cause flood peaks to arrive simultaneously
Coincident tributary peaks
Produces unusually high flows at confluences
High downstream water levels
Creates backwater and reduces drainage efficiency
Tides and storm surge
Can impede discharge from coastal watersheds
Natural sediment transport
Gradually changes channel and reservoir capacity
Natural channel migration/erosion
Alters conveyance and can threaten development
Naturally high groundwater
Reduces infiltration and drainage capacity
For Houston, flat terrain deserves special emphasis. A relatively small change in downstream water level, sediment accumulation, subsidence, obstruction, or discharge can propagate upstream as backwater because there isn’t much gravitational head available to overcome it.
2. WHAT WE DO — Human Actions that Increase Flood Risk
These can be divided into five mechanisms: more runoff, less storage, less conveyance, altered timing, and greater exposure.
Human action
Primary mechanism
Add impervious cover
↑ Runoff volume and peak
Clear vegetation
↑/accelerates runoff
Compact soils during development
↓ Infiltration
Install efficient storm sewers
Accelerates concentration
Drain natural depressions
↓ Storage
Destroy/fill wetlands
↓ Storage/infiltration
Fill floodplains
↓ Flood storage
Build in floodways
↓ Conveyance
Encroach on channels
↓ Conveyance
Undersize culverts
Creates bottlenecks/backwater
Undersize bridges/openings
Creates bottlenecks/backwater
Elevate roads with inadequate cross-drainage
Creates barriers to overland flow
Channelize/straighten streams
Accelerates downstream flow
Construct levees
Redistributes floodwater/removes storage
Build inadequate detention
↑ Downstream runoff
Release detention at unfavorable times
Causes peak stacking
Make reservoir releases during downstream peaks
Adds to downstream peak
Operate reservoirs independently
Can synchronize peaks
Withdraw excessive groundwater
Causes subsidence
Mine sand in active floodplains/floodways
Can alter channels, erosion and sediment movement
Allow excessive construction erosion
↑ Sediment load
Discharge sediment into waterways
↓ Conveyance/storage
Dump debris into drainage systems
↓ Conveyance
Build in flood-prone areas
↑ Exposure
Put critical infrastructure in flood-prone areas
↑ Consequences
Continue development upstream of constrained channels
↑ Runoff delivered to existing bottlenecks
This category contains an important concept. A project can make flooding worse by changing where the water goes, how fast it gets there, when it arrives, or how much room is available for it when it gets there.
3. WHAT WE FAIL TO DO — Human Omissions that Allow Flood Risk to Increase
This category captures institutional and cumulative failure, not simply engineering mistakes.
Failure to understand changing risk
Failure
Consequence
Fail to update rainfall criteria
Infrastructure designed for obsolete rainfall assumptions
Don’t enforce construction Best Management Practices
Sediment enters waterways
Don’t inspect permitted facilities
Problems remain undetected
Don’t correct known violations
Violations become effectively permanent
Grant repeated variances/exceptions
Standards gradually lose effectiveness
Failure to mitigate known problems
Failure
Consequence
Don’t fix known bottlenecks
Predictable flooding continues
Don’t enlarge undersized crossings
Backwater persists
Don’t preserve floodplain
Natural storage disappears
Don’t preserve wetlands
Natural attenuation disappears
Don’t acquire repeatedly flooded properties
Known exposure continues
Don’t complete mitigation projects
Residents remain exposed
Don’t fund maintenance
Infrastructure deteriorates
Don’t fund mitigation proactively
Recovery substitutes for prevention
Don’t adapt infrastructure after major floods
Previous vulnerabilities remain
Failure to coordinate
Failure
Consequence
Jurisdictions plan independently
Upstream actions impose downstream consequences
Reservoirs operate independently
Releases can stack
Counties use different standards
Watershed protection becomes inconsistent
Cities/counties regulate only within boundaries
Hydrology ignores political boundaries
Agencies optimize individual projects
Basin-wide impacts can be overlooked
No watershed-wide authority
Nobody owns the cumulative problem
Conclusion
That last point deserves special attention in the San Jacinto Basin. Some political leaders have actually fought against creating a river-basin-wide flood authority.
But water follows topography, not jurisdictional boundaries. A watershed fragmented among cities, counties, drainage districts, flood-control districts, groundwater districts, river authorities, state agencies and federal agencies creates opportunities for individually defensible decisions to produce collectively undesirable outcomes.
Flood disasters rarely have a single cause. They are usually the product of natural extremes interacting with decades of accumulated human actions and omissions.
And that distinction matters enormously when discussing responsibility. We cannot prevent extreme rainfall. But rainfall alone does not determine how high the water gets, where it goes, how many people are exposed, or how much damage results.
When floods happen, the sheer length of this list encourages finger pointing by those wishing to evade their own responsibility.
9/13/2026 – Today is the 18th anniversary of Hurricane Ike, whose eye passed directly over Kingwood.
It got me wondering. How many storms have caused significant flooding somewhere in the seven-county Houston/Galveston Region since 2008? Short answer – 24, including 14 tropical and 10 non-tropical. For details and implications, read on.
Caveats on Search
ChatGPT helped. It reviewed a dozen websites, including the National Weather Service, NOAA, FEMA, Harris County Flood Control District (HCFCD), and news sites such as ReduceFlooding, ABC13, Click2Houston, Houston Chronicle, and Rice University’s Baker Institute.
The tropical category had a clear threshold, but non-tropical events were more judgment-dependent. If you included every storm known to have flooded at least a few homes, the count would rise. But 10 is defensible if the threshold is “significant flood damage.”
Tropical Events Affecting Houston Region Since 2008
Of the 14 tropical events, five were especially consequential: Ike, Harvey, Imelda, Nicholas, and Beryl. See the entire list below.
Year
Dates
Storm
Classification
Principal Houston Area Affected
2008
Aug. 5
Edouard
Tropical Storm
Landfall near McFaddin Wildlife Refuge; wind and rain across the Houston–Galveston region
2008
Sept. 12–13
Ike
Hurricane, Category 2
Landfall near Galveston; destructive wind, surge, widespread flooding
2015
June 16–17
Bill
Tropical Storm
Coastal flooding, storm surge, rainfall; minor flooding in portions of Harris and Galveston
2017
June 21–22
Cindy
Tropical Storm
Minor coastal flooding on Galveston and Bolivar Peninsula; rain in eastern portions of region
2017
Aug. 25–30
Harvey
Hurricane, Category 4 at initial Texas landfall
Catastrophic rainfall and river, bayou and reservoir flooding throughout metropolitan Houston
2019
Sept. 17–19
Imelda
Tropical Storm
Extreme rainfall, flooding, especially NE Harris, SE Montgomery, Liberty and Chambers counties
2020
June 6–8
Cristobal
Tropical Storm
Elevated tides, high surf and coastal flooding along Upper Texas Coast
2020
July 24–26
Hanna
Hurricane, Category 1
Outer rainbands, gusty winds, high surf and coastal effects
2020
Aug. 26–27
Laura
Hurricane, Category 4
Wind, surge, coastal effects, principally in Chambers and far eastern Liberty counties
2020
Sept. 20–23
Beta
Tropical Storm
Prolonged rainfall, street and coastal flooding, particularly south and southeast of Houston
2021
Sept. 13–14
Nicholas
Hurricane, Category 1
Landfall near Sargent; strong winds, heavy rain, coastal flooding, wide power outages
2024
June 18–20
Alberto
Tropical Storm
High surf, elevated tides and coastal flooding along Galveston Island and Bolivar Peninsula
2024
46211
Beryl
Hurricane, Category 1
Direct passage across metro area; damaging winds, flooding, tornadoes, extensive power outages
2024
Sept. 10–11
Francine
Hurricane, Category 2 at Louisiana landfall
High surf, elevated tides and relatively minor coastal effects on the Upper Texas Coast
Non-Tropical Events Affecting Houston Region Since 2008
Significant non-tropical events included:
Year
Date(s)
Event
Principal Area and Effects
2009
April 27–28
West Houston flood
Extreme short-duration rainfall; hundreds of homes flooded along Brays Bayou, Buffalo Bayou and Langham Creek; serious road flooding
2012
January 9
January severe-storm flood
Intense rain flooded homes and roads around Mission Bend, southwest Houston, Pearland and portions of Brazoria County; accompanied by tornadoes
2012
July 9–10
North Harris County flood
Slow-moving thunderstorms flooded more than 70 structures and numerous roads, especially in northern Harris County
2015
May 13–14
Clear Lake/Pre-Memorial Day flood
Homes and roads flooded in Clear Lake, Pasadena, Friendswood and southeastern Harris County; at least one death
2015
May 25–26
Memorial Day Flood
Approximately 6,000 homes flooded in Harris County; severe flooding along Brays, Buffalo and White Oak bayous; seven flood-related deaths
2015
October 30–31
Halloween Flood
Several hundred homes damaged or flooded across the Houston region; major road flooding and fatalities
2016
April 17–18
Tax Day Flood
More than 7,000 homes and roughly 2,700 apartment units flooded; extreme rainfall in western and northwestern Harris County; nine deaths
2016
May 26–June 3
Memorial Day/Brazos River Flood
Major river flooding in Fort Bend, Brazoria, Waller and Montgomery counties; hundreds of homes affected, evacuations and fatalities
2019
May 7–9
Kingwood–Elm Grove flood
Approximately 200 homes flooded in Elm Grove and North Kingwood Forest; widespread street and drainage flooding elsewhere
2024
April 28–May 5
San Jacinto–Trinity River flood
Repeated thunderstorms produced major flooding along the East and West Forks of the San Jacinto; hundreds rescued, homes inundated and communities evacuated
Key Conclusions
The central takeaway: Houston’s flooding is not solely a hurricane problem. It is a a heavy rainfall and drainage problem that hurricanes sometimes magnify.
A few other conclusions stand out:
Non-tropical storms matter as much as named storms. They occur approximately every other year.
Houston can flood in almost any month — not just during hurricane season. Flood preparedness and drainage maintenance must be year-round activities.
Ordinary-looking thunderstorms can become extraordinary disasters. Memorial Day and Tax Day floods demonstrate that a stalled line of thunderstorms can flood thousands of structures.
Floods cluster rather than arrive at orderly intervals. The phrase “100-year flood” does not mean residents receive 99 safe years between events.
Rainfall intensity, location and timing often matter more than the regional total. San Jacinto headwaters can cause devastating local damage while much of the metropolitan area remains relatively unaffected.
Different mechanisms produce different floods: street flooding, bayou/river overflow, reservoir flooding, storm surge and runoff from adjacent development. No single project or agency can address all of them.
Homes can flood even when relatively little rain falls directly over them. Rainfall in Montgomery, Liberty, Waller or other upstream counties can arrive later as riverine flooding.
Development decisions can convert a localized storm into a neighborhood disaster as the May 2019 Elm Grove flood illustrates.
The absence of a recent catastrophic floods does not demonstrate that the system has been fixed. Since Harvey, Houston has still experienced Imelda, Beta, Nicholas, the May 2019 flood, the 2024 San Jacinto flood and Beryl.
Each type of flooding exploits a different weakness in a fragmented regional system.
What the Region Needs
The region needs coordinated watershed governance, conservative development standards, adequate detention, drainage maintenance, updated rainfall assumptions, floodplain preservation, warning systems and projects designed around cumulative river basin behavior.
Posted by Bob Rehak on 9/13/2026
3302 Days since Hurricane Harvey and 18 years since Ike
https://i0.wp.com/reduceflooding.com/wp-content/uploads/2024/05/20240503-20240503_164539.jpg?fit=1100%2C508&ssl=15081100adminadmin2026-09-13 22:10:262026-09-13 22:29:23How Many Storms Caused Significant Houston Flooding Since Ike?
Flood-Mitigation Solutions Summarized
9/16/2026 – In my previous post, I summarized causes of flooding. I grouped 83 contributing factors into three main categories: nature, things humans do, and things humans fail to do. In my continuing effort to summarize years of research, today, I would like to summarize major categories of flood-mitigation solutions.
Major Categories of Flood-Mitigation Solutions
Flood mitigation is fundamentally about managing water better and reducing human vulnerability as development expands throughout watersheds. Below, I have grouped solutions into several major categories to make them easier to comprehend and remember. Each category lists multiple specific solutions within it that I have previously posted about.
1. Reduce runoff at the source
Keep rainfall from quickly becoming runoff. Preserve forests and natural areas. Limit unnecessary impervious cover with green alternatives, such as permeable pavement, rain gardens, bio-swales, green roofs, soil restoration, infiltration practices, and development standards that control post-development runoff.
While particularly useful for moderate storms, during extreme events, soils and small-scale storage can easily become saturated. So, view them as one layer of protection.
2. Preserve natural storage
This is almost always cheaper than trying to recreate storage after development.
Protect floodplains, wetlands, natural depressions, riparian corridors and other areas where water can temporarily spread without causing substantial damage.
The fundamental principle is:
3. Detain or retain excess runoff
Where development has already increased runoff, temporarily store the excess.
Solutions include detention basins, regional detention facilities, retention ponds, wetlands, underground storage and flood-control reservoirs. But don’t evaluate storage solely by acre-feet. Its location, outlet capacity and release timing also matter. A detention basin that releases water at the wrong time can contribute to downstream peaks.
4. Improve conveyance
Once water enters the drainage network, there must be enough capacity to move it safely.
Solutions include larger storm sewers, additional inlets, larger culverts, bridge modifications, ditch improvements, channel widening, selective channel excavation, bypass channels, diversion channels, flood tunnels and—in appropriate circumstances—dredging.
But there’s an important caveat:
Improving conveyance upstream without considering downstream capacity can simply transfer the flood problem downstream.
5. Remove bottlenecks
The weakest link in a drainage system limits the entire system’s effectiveness.
A watershed may have ample channel capacity except for one undersized bridge, culvert, railroad crossing, utility crossing, sediment deposit or other constriction. This is especially important in an area, such as Houston, with flat terrain.
6. Manage sediment
Sediment management is especially relevant to the San Jacinto/Lake Houston system.
Possible mitigation measures include erosion prevention, construction-site BMP enforcement, stream-bank stabilization, better sand-mining practices, setbacks from channels, protection against pit capture, sediment traps where appropriate, dredging, and maintaining critical channel and tributary-mouth conveyance.
The objective: prevent excessive human-caused sedimentation from reducing critical conveyance or storage.
7. Manage flood peaks better
When water arrives affects flood peaks as much as how much arrives.
Potential solutions include coordinated reservoir operations, coordinated detention releases, strategically located regional detention, watershed-scale hydrologic modeling, real-time rainfall/stream monitoring, forecast-informed operations and—in some circumstances—pre-releases.
The goal: to avoid peaks from multiple tributaries, detention systems and reservoirs arriving at the same location at approximately the same time and stacking on each other.
8. Protect structures
Where development already exists in locations that have become hazardous, take steps to protect structures.
Examples include home elevation, floodproofing, floodwalls, levees, berms, gates, pumps, backflow prevention, elevated utilities and protection of critical facilities.
These measures generally reduce damage rather than eliminate flooding. But understand that a levee or floodwall, like the one at Kingwood High School, can reduce risk without making the protected area flood-proof.
9. Remove development from and/or stop developing in the highest-risk locations
Sometimes the most durable flood-control is simply to stop putting valuable things where water wants to go repeatedly.
Measures include voluntary buyouts, property acquisition, conversion of repetitive-loss areas to open space, preventing redevelopment of acquired properties, stricter floodway development restrictions, and avoiding new critical facilities in flood-prone areas.
This attacks exposure rather than hydraulics. But it protects people and property. Local examples include the buyout of townhomes in Forest Cove and efforts to block the proposed development of homes where Cypress, Spring and Turkey Creeks join the San Jacinto West Fork.
10. Maintain the drainage system
Maintenance is one of the least glamorous and most important mitigation strategies.
Maintain channels, storm sewers, inlets, culverts, detention basins, pumps, gates and outfalls; remove debris and problematic sediment; repair erosion; inspect infrastructure; and preserve the designed storage and conveyance capacity.
A drainage system’s capacity should not be considered fixed at the capacity it had when constructed.
Without maintenance, design capacity deteriorates and flood risk increases.
11. Enforce the rules already on the books
New regulations accomplish little if existing ones aren’t enforced.
That includes floodplain/floodway restrictions, detention requirements, no-net-fill requirements, construction BMPs, stormwater permits, wetland requirements, mining permits, drainage easements and development conditions.
Effective enforcement goes beyond permitting. It requires inspection, documentation and correction when violations occur.
12. Design for tomorrow’s watershed
Flood infrastructure often lasts many decades. Designing only for today’s watershed can lock in future problems.
Planning should consider growth of impervious cover, upstream development, updated rainfall probabilities, subsidence, land-use change, downstream constraints and reasonably foreseeable changes in watershed hydrology.
This means building in generous safety margins. Development projects should do more than meet minimum requirements. They should still keep residents safe as the watershed develops.
13. Coordinate across the river basin
Floodwaters don’t recognize municipal or county boundaries. Effective mitigation therefore requires shared rainfall assumptions, compatible design standards, watershed-wide models, coordinated detention, reservoir operations, development assumptions, sediment management and capital planning.
It also requires a single accountable authority to “own” problems. Otherwise one jurisdiction’s successful drainage project can become another jurisdiction’s increased inflow.
14. Improve forecasting, warning and preparedness
These actions don’t prevent flooding. But they can dramatically reduce its consequences…as we learned in the Hill Country flooding at Camp Mystic.
Better rainfall forecasts, stream gauges, reservoir gauges, inundation forecasts, warning systems, evacuation planning, emergency communications and public education can save lives and property.
Posted by Bob Rehak on 9/16/26
3305 Days since Hurricane Harvey
Causes of Flooding Summarized
9/14/2026 – “Causes of flooding summarized” is part of my continuing effort to boil down more than 2 million words in 3100 posts since Hurricane Harvey into short summaries of key topics. I’ve seen the 83 causes of flooding listed below happen over and over again in different places in different combinations at different times. With the help of ChatGPT, I’ve organized them into three main groupings: Nature, What Humans Do, and What We Fail to Do.
The Three Large Groupings
1. NATURE — Conditions We Largely Cannot Control
These establish the underlying hydrologic and hydraulic setting.
For Houston, flat terrain deserves special emphasis. A relatively small change in downstream water level, sediment accumulation, subsidence, obstruction, or discharge can propagate upstream as backwater because there isn’t much gravitational head available to overcome it.
2. WHAT WE DO — Human Actions that Increase Flood Risk
These can be divided into five mechanisms: more runoff, less storage, less conveyance, altered timing, and greater exposure.
This category contains an important concept. A project can make flooding worse by changing where the water goes, how fast it gets there, when it arrives, or how much room is available for it when it gets there.
3. WHAT WE FAIL TO DO — Human Omissions that Allow Flood Risk to Increase
This category captures institutional and cumulative failure, not simply engineering mistakes.
Failure to understand changing risk
Failure to maintain
Failure to regulate and enforce
Failure to mitigate known problems
Failure to coordinate
Conclusion
That last point deserves special attention in the San Jacinto Basin. Some political leaders have actually fought against creating a river-basin-wide flood authority.
But water follows topography, not jurisdictional boundaries. A watershed fragmented among cities, counties, drainage districts, flood-control districts, groundwater districts, river authorities, state agencies and federal agencies creates opportunities for individually defensible decisions to produce collectively undesirable outcomes.
Flood disasters rarely have a single cause. They are usually the product of natural extremes interacting with decades of accumulated human actions and omissions.
And that distinction matters enormously when discussing responsibility. We cannot prevent extreme rainfall. But rainfall alone does not determine how high the water gets, where it goes, how many people are exposed, or how much damage results.
When floods happen, the sheer length of this list encourages finger pointing by those wishing to evade their own responsibility.
Avoiding floods requires everyone to do their part and avoid creating an adverse impact for others.
Posted by Bob Rehak on 9/14/2026
3303 Days since Hurricane Harvey
How Many Storms Caused Significant Houston Flooding Since Ike?
9/13/2026 – Today is the 18th anniversary of Hurricane Ike, whose eye passed directly over Kingwood.
It got me wondering. How many storms have caused significant flooding somewhere in the seven-county Houston/Galveston Region since 2008? Short answer – 24, including 14 tropical and 10 non-tropical. For details and implications, read on.
Caveats on Search
ChatGPT helped. It reviewed a dozen websites, including the National Weather Service, NOAA, FEMA, Harris County Flood Control District (HCFCD), and news sites such as ReduceFlooding, ABC13, Click2Houston, Houston Chronicle, and Rice University’s Baker Institute.
The tropical category had a clear threshold, but non-tropical events were more judgment-dependent. If you included every storm known to have flooded at least a few homes, the count would rise. But 10 is defensible if the threshold is “significant flood damage.”
Tropical Events Affecting Houston Region Since 2008
Of the 14 tropical events, five were especially consequential: Ike, Harvey, Imelda, Nicholas, and Beryl. See the entire list below.
Non-Tropical Events Affecting Houston Region Since 2008
Significant non-tropical events included:
Key Conclusions
The central takeaway: Houston’s flooding is not solely a hurricane problem. It is a a heavy rainfall and drainage problem that hurricanes sometimes magnify.
A few other conclusions stand out:
What the Region Needs
The region needs coordinated watershed governance, conservative development standards, adequate detention, drainage maintenance, updated rainfall assumptions, floodplain preservation, warning systems and projects designed around cumulative river basin behavior.
Posted by Bob Rehak on 9/13/2026
3302 Days since Hurricane Harvey and 18 years since Ike