Partial Kingwood Diversion Ditch Funding Up For Approval Thursday

10/12/26 – Harris County Flood Control District (HCFCD) has 44 items on the 10/15/26 Commissioners Court Agenda. Among them, a request to approve a $5 million grant from the Texas Water Development Board (TWDB) for drainage improvements to the Kingwood Diversion Ditch. See Item 432.

TWDB authorized the grant to HCFCD in January this year. State Rep. Charles Cunningham obtained it during the 89th Legislative Regular Session. By itself, the $5 million won’t come close to funding the entire Diversion Ditch Project. But it will play an important part in the larger funding picture.

On 3/26/26, former HCFCD Executive Director Dr. Tina Petersen, told the San Jacinto River Authority Board that the entire project will cost approximately $43 million and is fully funded through construction. At the time, Petersen estimated that construction would start in April 2027 and finish before the end of 2027.

Scope, Location Funding of Project

The scope includes four bridge replacements, a new diversion structure, 4.2 miles of channel work, and a new outfall that bypasses River Grove Park. See Page 18 of Petersen’s presentation.

Bens Branch and Kingwood Diversion Ditch
Red Diagonal = Bens Branch. White = Kingwood Diversion Ditch. Green = new outfall to river.

Additional funding for Diversion Ditch improvements will come from Congressman Dan Crenshaw’s 2023 earmark to replace the Walnut Lane Bridge shown below. Crenshaw’s earmark helped rescue the project from oblivion  in 2025 when the Democratic members of Harris County Commissioners Court passed a motion to reallocate all funding from projects that fell below the top quartile of their equity prioritization framework to projects in the top quartile.

However, Precinct 3 Commissioner Tom Ramsey PE warned of unintended consequences associated with that plan, i.e., the loss of federal funding already committed, such as Crenshaw’s. Crenshaw requested the funding in 2023. Congress awarded it in 2024. 

Dan Crenshaw on Walnut Lane Bridge over Kingwood Diversion Ditch
U.S. Rep. Dan Crenshaw gives the thumbs up to the Walnut Lane Bridge project. Widening the bridge is necessary to widen the Kingwood Diversion Ditch (background) which will also help reduce flood risk along Bens Branch.

Diverting water from Bens Branch is important because Bens Branch runs through Kingwood Town Center where 12 people died from Harvey flooding.

Kingwood Diversion Ditch
Looking N toward Kingwood Drive from over the Walnut Lane Bridge.

Complementary Project

The Lake Houston Redevelopment Authority/TIRZ 10, also plans to build a detention basin and expand the Diversion Ditch north of Northpark Drive in Montgomery County. Spending Harris County money outside Harris County has encountered political resistance among some Harris County Commissioners in the past even though it could save Harris County lives.

Kingwood Diversion Ditch Detention Project for Northpark Expansion
LHRA/TIRZ 10 Project T-1015 complement HCFCD efforts

Posted by Bob Rehak on 10/12/26

3331 Days since Hurricane Harvey

What Causes Hurricanes to Form, Strengthen and Weaken?

10/10/26 – After a life measured in days, Hurricane Isaias went from an area of low pressure in the Bay of Campeche to a killer, Cat 3 hurricane to a post-tropical storm now causing flash flooding in the Appalachians. So, what forces cause hurricanes to form, strengthen and weaken?

I dedicate this post to curious readers and budding scientists still in school. Please share it with your students, children and grandchildren.

What Causes Hurricanes to Form?

The forces listed below support formation of an organized tropical cyclone.

Key force or conditionWhat happens physicallyEffect on the developing storm
An existing weather disturbanceThunderstorms gather around a low-pressure area, such as a tropical wave.Provides the starting circulation around which a storm can organize.
Warm ocean waterThe ocean supplies heat and water vapor to air above it. Water temperatures around 80°F (27°C) generally favor development.Supplies energy for sustained thunderstorms.
Moist airHumidity limits evaporation and cooling within developing thunderstorms.Helps thunderstorms persist and organize.
An atmosphere that supports rising airWarm, moist air rises, cools, and condenses, releasing heat.Builds deep thunderstorms that help strengthen the circulation.
Low vertical wind shearWinds change relatively little with height, allowing the lower and upper circulation to remain aligned.Helps thunderstorms organize around the surface center.
Sufficient distance from the equatorEarth’s rotation deflects moving air through the Coriolis effect.Helps organize a rotating circulation; tropical cyclones rarely form within about 5 degrees of the equator.

These conditions favor formation, but their presence does not guarantee that a hurricane will develop. Sources: NOAA’s hurricane overview and formation explanation. www.noaa.gov.

Warm, moist air flows inward over the ocean and rises in thunderstorms. An organized hurricane develops a central eye, and outflow high above the storm. Source: NOAA

What Causes Hurricanes to Strengthen?

Once a tropical storm develops, alignment of the conditions below can intensify it into a hurricane (sustained winds 74 mph or greater).

Key force or conditionWhat happens physicallyEffect on the hurricane
A continuing supply of ocean heat and moistureSurface air picks up heat and water vapor, then carries that energy into the eyewall.Fuels stronger thunderstorms and circulation.
Warm water extending deep below the surfaceWind-driven mixing brings up relatively warm water instead of quickly exposing cold water.Sustains the energy supply as the hurricane churns the ocean.
Concentrated heating in the eyewallRising water vapor condenses and releases heat close to the center.Strengthens the warm core and helps central pressure fall, increasing winds.
Low or no vertical wind shearThe circulation remains more vertically aligned.Allows eyewall thunderstorms to organize and heat the core efficiently.
Moist surrounding airLess dry air enters and disrupts eyewall updrafts.Helps maintain vigorous thunderstorms around the center.
Effective outflow aloftAir rising through the eyewall spreads outward near the top of the storm.Supports the continuing flow of air inward below and upward through the eyewall.
An increasingly organized inner coreThunderstorms form a more continuous eyewall; the eyewall may contract.Concentrates the strongest circulation closer to the center and can accelerate strengthening.
Low wind shear lets circulation remain vertically aligned, helping thunderstorms concentrate heat around the center and favoring strengthening. Contrast this image with the one below. Source: NOAA

Sources: NOAA’s ocean conditions research and hurricane modeling explanation.

What Causes Hurricanes to Weaken?

These conditions cause hurricanes to weaken as they move.

Key force or conditionWhat happens physicallyEffect on the hurricane
Strong vertical wind shearWinds at different heights tilt the circulation and displace thunderstorms from the surface center.Disrupts the organized eyewall and reduces heating of the core.
Dry air entering the inner coreEvaporation cools air within thunderstorms, encouraging downdrafts and interrupting moist updrafts.Erodes eyewall thunderstorms and can open gaps in the eyewall.
Cooler ocean waterLess heat and water vapor transfer from the ocean to the atmosphere.Reduces the energy available to sustain the hurricane.
Cold water mixed upward by the stormStrong winds churn the ocean and can bring colder water to the surface.Allows the hurricane to weaken its own energy supply, especially over a shallow warm layer.
LandfallAccess to ocean heat and moisture diminishes; surface friction increases, and terrain can disrupt circulation.Slows winds and breaks down the eyewall, although heavy rain can persist.
An eyewall replacement cycleAn outer eyewall develops and intercepts inflow feeding the original eyewall, which weakens and disappears.Often temporarily lowers maximum winds while expanding the wind field; strengthening may resume.
Strong wind shear tilts the circulation and disrupts the organized flow of heat and moisture, inhibiting development and potentially weakening the storm. Landfall, dry air, and cooler water also cause weakening.  Source: NOAA.

Isaias encountered wind sheer shortly before reaching land. That lowered its intensity at landfall from Cat 3 to Cat 2.

Sources: NOAA’s satellite interpretation guide, hurricane FAQ, and eyewall research.

Effect on Flooding

Note that “strengthening” and “weakening” usually describe changes in maximum sustained winds. A weakening hurricane can still produce destructive storm surge and prolonged, intense rainfall. Hurricane Harvey is an excellent example.

In 2017, Harvey’s winds weakened dramatically before much of Houston’s catastrophic flooding occurred. The National Weather Service documents the sequence below.

StageWhat happened
Landfall, August 25Harvey struck near Rockport as a Category 4 hurricane with 130 mph sustained winds.
Weakening, August 26It weakened to a tropical storm within approximately 12 hours, then maintained winds around 40 mph for the next couple of days.
Prolonged floodingWeak steering currents caused Harvey to stall near the coast. Part of its circulation remained over the Gulf, sustaining its moisture supply and repeated torrential rainfall.

The results were extraordinary:

The key point: Harvey weakened as a windstorm, but remained a catastrophic rainstorm.

A lower hurricane category does not necessarily mean a lower flood threat.

In fact, Harvey produced the highest recorded rainfall total ever from a single tropical cyclone in the continental United States: 60.58 inches near Nederland, Texas, according to the National Weather Service.

Posted by Bob Rehak on 10/10/2026

3329 Days since Hurricane Harvey

Isaias Now a Major Hurricane

10/9/26 @ 10AM – This morning, Hurricane Isaias intensified into a major Category 3 Hurricane with sustained winds of 120 mph. Isaias should make landfall near Pensacola late tonight or early tomorrow morning, according to the National Hurricane Center.

Increasing forward motion should bring strong winds far inland over the southeast U.S. into the Tennessee and Ohio River Valleys, causing widespread power outages.

The National Hurricane Center (NHC) expects tropical-storm-force winds to arrive on the Florida panhandle by 2PM today.

Arrival Time

Tropical-storm-force winds now extend outward 185 miles from the center and hurricane force winds 30 miles.

Damaging wind gusts are possible over much of central and northern Alabama, extreme eastern Mississippi, and portions of western and northern Georgia, especially in areas of higher terrain.

Rainfall and Flooding Potential

Isaias will bring areas of heavy rainfall to the central U.S. Gulf coast and much of the Southeast through the weekend.

Considerable flash and urban flooding, along with significant river flooding, will be possible.

Storm Surge Up to 9 Feet

NHC predicts damaging storm surge up to 9 feet in the western Florida Panhandle, with lesser amounts elsewhere.

Maximum values will occur near and to the east of where the center crosses the coast.  

Infrared satellite images show an eye surrounded by intense thunderstorms.

Infrared satellite image as of 9:16 CDT this morning

Tropical Tidbits shows this animated IR Satellite Loop. However, an eye is not apparent on the Geo-Color view.

Near Peak, but Increasing Forward Speed and Wind-Field Width

The hurricane is passing over a warm deep water eddy and that is likely helping the intensification process in the face of increasing vertical shear. Isaias has turned toward the NNE and is increasing in forward speed.

Isaias is likely near peak. However, it is possible that the hurricane could intensify a bit more this morning before strong shear begins to impact the system.

The wind field will greatly expand later today into tonight as Isaias makes landfall and moves inland while interacting with an upper level trough to the west.

Origin of Name

Isaias is pronounced “ees-ah-EE-ahs” – four syllables – with the emphasis on the third. That is NHC’s official pronunciation. 

According to ChatGPT, Isaías is the Spanish and Portuguese form of Isaiah, the biblical prophet’s name. It comes from Hebrew Yesha‘yahu, meaning “Yahweh is salvation,” or “salvation of the Lord.” 

Why use a name that English speakers may find difficult? NHC follows name lists maintained by the World Meteorological Organization’s (WMO) Hurricane Committee. Atlantic lists deliberately balance English, French and Spanish names because storms affect countries speaking all three languages. The lists rotate every six years. Isaias replaced Ike after the destructive 2008 hurricane caused Ike’s name to be retired. NOAA

WMO itself says storm names should be instantly recognizable for safety. The multilingual approach explains the choice, although it clearly creates a pronunciation hurdle for many English speakers.

Posted by Bob Rehak on 10/9/26 based on information from NHC and Harris County Meteorologist Jeff Lindner

3328 Days since Hurricane Harvey