National Water Recovery

Harvey 2017 · NOAA Stage IV + USGS WBD

Gross rainfall by pilot watershed

Seven daily NOAA rainfall grids, ending August 26 through September 1, 2017, were intersected with USGS watershed polygons. The first ledger covers five HUC8 basins and their 139 HUC12 subwatersheds in the San Jacinto and Lower Brazos areas.

Rainfall is not recoverable water. Acre-feet below are precipitation over land, before infiltration, evaporation, ordinary river flow, downstream rights, intake limits, water quality and recharge constraints. Do not treat them as supply or add them to the older 71.5 MAF screening footprint.

Five pilot basins

Gross volumes are calculated from fractional raster-cell overlap. All five basins have 100% valid grid coverage to the displayed precision.

HUC8BasinArea (km²)Mean rain (in.)Gross rain (acre-ft)HUC12s
12040101West Fork San Jacinto2,80122.391,291,80625
12040102Spring1,96029.211,179,01520
12040103East Fork San Jacinto2,57727.171,441,74825
12040104Buffalo-San Jacinto3,06336.152,279,76428
12070104Lower Brazos4,25524.942,185,54141

139 subwatershed records

Open a basin to inspect its HUC12 codes, rainfall depth, gross volume and complete-grid coverage. HUC12 totals reconcile to each HUC8 total within one acre-foot after rounding.

West Fork San Jacinto · 12040101 · 25 subwatersheds +
HUC12NameMean rain (in.)Gross acre-ftCoverage
120401010101Rocky Creek-West Fork San Jacinto River20.7263,435100.00%
120401010102McGary Creek20.8728,604100.00%
120401010103West Sandy Creek20.6347,227100.00%
120401010104Robinson Creek-West Fork San Jancinto River21.3452,485100.00%
120401010201East Sandy Creek20.3526,169100.00%
120401010202McDonald Creek-West Fork San Jacinto River20.9563,465100.00%
120401010203Caney Creek19.2741,557100.00%
120401010204Hostetter Creek-Lake Conroe20.4466,624100.00%
120401010205Little Lake Creek-Lake Conroe20.0152,592100.00%
120401010206Town Creek-Lake Conroe20.8251,124100.00%
120401010207White Oak Creek-West Fork San Jacinto River22.8844,379100.00%
120401010301Flagtail Creek-Lake Creek18.0547,337100.00%
120401010302Garretts Creek18.2830,514100.00%
120401010303Kidhaw Branch-Lake Creek20.0839,297100.00%
120401010304Haynie Creek-Little Caney Creek19.9038,679100.00%
120401010305Sand Creek-Caney Creek20.6341,352100.00%
120401010306Town of Dobbin-Lake Creek22.3634,028100.00%
120401010307Landrum Creek-Lake Creek23.2465,360100.00%
120401010308Mound Creek-Lake Creek23.0073,972100.00%
120401010401Stewarts Creek-West Fork San Jacinto River22.6439,639100.00%
120401010402Little Caney Creek-West Fork San Jacinto River23.4039,039100.00%
120401010403Crystal Creek21.3654,924100.00%
120401010404Black Slough-West Fork San Jacinto River28.0687,537100.00%
120401010501Bens Branch32.16100,717100.00%
120401010502San Jacinto Dam35.0661,750100.00%
Spring · 12040102 · 20 subwatersheds +
HUC12NameMean rain (in.)Gross acre-ftCoverage
120401020101Mound Creek-Cypress Creek29.9071,813100.00%
120401020102Live Oak Creek29.2329,363100.00%
120401020103Mallard Lake-Cypress Creek33.23103,248100.00%
120401020104Dry Creek-Cypress Creek35.2858,780100.00%
120401020105Little Cypress Creek32.1092,642100.00%
120401020106Marshall Lake-Cypress Creek30.0187,581100.00%
120401020107Turkey Creek-Cypress Creek31.4093,737100.00%
120401020201Kickapoo Creek-Spring Creek28.0751,531100.00%
120401020202Threemile Creek-Brushy Creek28.3374,286100.00%
120401020203Birch Creek-Walnut Creek27.4053,810100.00%
120401020204Mink Branch-Walnut Creek28.6958,990100.00%
120401020205Sugar Creek-Spring Creek29.2449,906100.00%
120401020206Hurricane Creek-Mill Creek25.1435,023100.00%
120401020207Kachel Lake-Mill Creek26.1625,982100.00%
120401020208Decker Branch-Mill Creek25.6141,654100.00%
120401020209Dry Creek-Spring Creek25.2153,927100.00%
120401020210Willow Creek28.0582,388100.00%
120401020211Bear Branch-Panther Branch25.1737,138100.00%
120401020212Panther Branch-Spring Creek26.8241,968100.00%
120401020213Spring Creek32.5135,249100.00%
East Fork San Jacinto · 12040103 · 25 subwatersheds +
HUC12NameMean rain (in.)Gross acre-ftCoverage
120401030101Hegar Branch-Caney Creek21.3850,026100.00%
120401030102McRae Creek-Caney Creek22.0556,860100.00%
120401030103West Fork Spring Branch-Spring Branch23.0645,722100.00%
120401030104Cagle Branch-Caney Creek22.9829,141100.00%
120401030105Dry Creek-Caney Creek26.1343,106100.00%
120401030106Boggy Creek-Peach Creek23.4859,933100.00%
120401030107Lawrence Creek-Peach Creek25.6448,081100.00%
120401030108Jayhawker Creek27.4033,788100.00%
120401030109Gully Branch-Peach Creek27.1371,952100.00%
120401030110White Oak Creek28.8649,238100.00%
120401030201Upper Tarkington Bayou28.4284,140100.00%
120401030202Marsh Branch-Tarkington Bayou32.1174,849100.00%
120401030203Lower Tarkington Bayou35.9452,749100.00%
120401030204Indian Gulley-Luce Bayou41.4988,192100.00%
120401030205Luce Bayou34.9185,660100.00%
120401030301Boswell Creek24.5930,975100.00%
120401030302Gourd Creek-Winters Bayou22.4173,611100.00%
120401030303Hopkins Branch-Winters Bayou24.3372,256100.00%
120401030304Nebletts Creek-Winters Bayou25.7441,205100.00%
120401030305Cobb Creek-East Fork San Jacinto River24.9063,547100.00%
120401030306McCombs Creek-East Fork San Jacinto River25.3323,215100.00%
120401030307Miller Creek-East Fork San Jacinto River24.1960,314100.00%
120401030308Oil Creek-East Fork San Jacinto25.0643,456100.00%
120401030401Whiskey Branch-East Fork San Jancito River30.4270,767100.00%
120401030402Orange Branch-East Fork San Jacinto River32.3088,966100.00%
Buffalo-San Jacinto · 12040104 · 28 subwatersheds +
HUC12NameMean rain (in.)Gross acre-ftCoverage
120401040101Willow Fork32.5666,845100.00%
120401040102Cane Island Branch34.7629,474100.00%
120401040103Little Prong-Buffalo Bayou33.5248,582100.00%
120401040104Barker Reservoir-Buffalo Bayou34.6996,676100.00%
120401040201Langham Creek35.44103,922100.00%
120401040202Bear Creek33.6259,387100.00%
120401040203South Mayde Creek33.4379,926100.00%
120401040301Jersey Lake-Whiteoak Bayou32.1139,459100.00%
120401040302Cole Creek-Whiteoak Bayou33.5592,060100.00%
120401040303Spring Branch-Buffalo Bayou34.4896,204100.00%
120401040304Little Whiteoak Bayou-Whiteoak Bayou34.8878,545100.00%
120401040305City of Houston-Buffalo Bayou34.2637,251100.00%
120401040401Keegans Bayou-Brays Bayou35.12179,626100.00%
120401040402Country Club Bayou-Brays Bayou35.4386,687100.00%
120401040501Upper Sims Bayou34.7985,070100.00%
120401040502Lower Sims Bayou40.36107,001100.00%
120401040601Headwaters Greens Bayou32.6358,337100.00%
120401040602Garners Bayou34.6063,969100.00%
120401040603Upper Greens Bayou34.7275,480100.00%
120401040604Halls Bayou37.48103,849100.00%
120401040605Middle Greens Bayou38.4038,158100.00%
120401040606Lower Greens Bayou40.5562,951100.00%
120401040701Hunting Bayou40.8488,893100.00%
120401040702Carpenters Bayou38.2677,181100.00%
120401040703Vince Bayou-Buffalo Bayou41.60132,178100.00%
120401040704Jackson Bayou-San Jacinto River37.84112,068100.00%
120401040705Highlands Reservoir-San Jacinto River38.7358,465100.00%
120401040706Goose Creek39.11121,521100.00%
Lower Brazos · 12070104 · 41 subwatersheds +
HUC12NameMean rain (in.)Gross acre-ftCoverage
120701040101Headwaters Caney Creek17.3231,769100.00%
120701040102Browning Branch-Brazos River16.4317,668100.00%
120701040103Gibbs Creek-Caney Creek17.2526,397100.00%
120701040104Ponds Creek-Clear Creek22.2956,016100.00%
120701040105Threemile Creek-Clear Creek22.7234,877100.00%
120701040106Lewisville Creek-Brazos River18.8228,313100.00%
120701040107Dry Creek-Piney Creek21.4244,975100.00%
120701040108Ives Creek-Brazos River21.2850,098100.00%
120701040201Indian Creek-East Mill Creek22.5047,919100.00%
120701040202Sandy Creek-East Mill Creek21.4530,727100.00%
120701040203Jackson Creek-East Mill Creek20.3540,395100.00%
120701040204East Mill Creek18.2753,619100.00%
120701040205Upper West Mill Creek21.4444,871100.00%
120701040206Middle West Mill Creek19.3952,953100.00%
120701040207Post Oak Point Creek-Sandy Creek20.3034,898100.00%
120701040208Lower West Mill Creek19.1433,692100.00%
120701040209Sandy Creek-Mill Creek22.2966,876100.00%
120701040210Deadman Creek-Mill Creek25.4171,449100.00%
120701040301Harris Creek-Irons Creek25.8642,860100.00%
120701040302Mulberry Creek-Irons Creek29.3437,749100.00%
120701040303Dry Branch-Bessies Creek31.5088,571100.00%
120701040304Bullinger Creek-Brazos River25.4638,667100.00%
120701040305Upper Allens Creek20.7037,642100.00%
120701040306Lower Allens Creek23.0242,132100.00%
120701040307Cannons Lake-Brazos River28.0146,008100.00%
120701040308Brookshire Creek-Bessies Creek31.4177,322100.00%
120701040309Cottonwood Creek-Brazos River28.5455,996100.00%
120701040401Sandy Branch-Brazos River29.4296,144100.00%
120701040402Rabbs Bayou-Brazos River33.4397,651100.00%
120701040403Steep Bank Creek-Brazos River36.7758,076100.00%
120701040404Coon Creek-Cottonwood Creek28.9148,205100.00%
120701040405Seabourne Creek-Big Creek29.0156,603100.00%
120701040406Fairchilds Creek-Big Creek29.4473,870100.00%
120701040407Worthington Lake-Big Creek30.5355,850100.00%
120701040408Dry Creek-Rabbs Bayou31.2968,012100.00%
120701040409Dry Bayou-Brazos River34.21104,169100.00%
120701040501Cow Creek-Brazos River29.7096,407100.00%
120701040502Varner Creek23.8066,212100.00%
120701040503Harris Reservoir-Brazos River23.7862,598100.00%
120701040504Middle Bayou-Brazos River17.7017,682100.00%
120701040505Outlet Barzos River16.6349,602100.00%

What USGS river gauges reported

Daily mean discharge from August 25 through September 10, a 17-day window that includes the flood tail. The table integrates published daily river flow past each gauge. It is a separate observation from the seven-day rainfall ledger above. Gauges have different contributing areas, so these totals cannot be summed or compared directly to the basin rainfall volumes.

USGS gaugeDays presentReported river flow (acre-ft)Estimated days
Brazos River near RosharonUSGS 0811665017/172,210,6380
West Fork San Jacinto above Lake Houston near PorterUSGS 0806809017/17657,7430
Spring Creek near SpringUSGS 0806850017/17373,2970
East Fork San Jacinto near New CaneyUSGS 0807020017/17477,5672
Buffalo Bayou at HoustonUSGS 0807400016/17 *423,7093

* Buffalo Bayou lacks August 25 in this export, so its volume is a 16-day partial total. USGS marks some daily means “A:e” as estimated. River flow contains ordinary and upstream water, plus reservoir operations; none of these totals is a storm-only runoff or divertible-water estimate.

Download daily gauge readings and quality flags

One observed river checkpoint

Lower Brazos pilot: capacity screen

USGS 08116650 near Rosharon, Texas, reports daily mean river flow from August 25 to September 10, 2017. Choose a hypothetical flow floor and intake capacity to see how much water a continuously operating intake could intercept at this gauge under daily-average arithmetic. This does not select an intake bank or a destination.

Assumed flow left at the gauge. This is not an adopted legal limit.

Assumed continuous pumping and conveyance rate; no equipment is specified.

Screening formula per day: min(intake capacity, max(0, daily mean discharge − assumed floor)) × 1.98347 acre-ft per cfs-day. A 24-hour mean cannot prove that rate could be sustained every hour.

Hypothetical gauge-side ceiling

23,802 acre-ft

12 of 17 days above the selected floor and with nonzero modeled intake.

The gauge reported 2,210,638 acre-ft of total river flow in the window and a peak daily mean of 121,000 cfs. Neither figure is storm-only water. The modeled ceiling is not an estimate of actual diversion, retained water, aquifer recharge, or water saved from the sea.
Date (2017)Observed daily mean (cfs)Screened ceiling (acre-ft)
2017-08-252,3300
2017-08-2617,8000
2017-08-2743,5001,983
2017-08-2871,6001,983
2017-08-29121,0001,983
2017-08-30117,0001,983
2017-08-31101,0001,983
2017-09-01101,0001,983
2017-09-02103,0001,983
2017-09-0398,1001,983
2017-09-0490,3001,983
2017-09-0578,2001,983
2017-09-0660,4001,983
2017-09-0744,5001,983
2017-09-0828,2000
2017-09-0920,2000
2017-09-1016,4000

The route is still an open engineering decision

No verified receiving parcel, storage or aquifer injection facility, alignment, intake design, permitted diversion, water-quality treatment, or receiving rate is in this pilot. A complete route volume and project cost therefore remain uncalculated. The next gate is to identify a specific receiving site and map the intake-to-site alignment, then obtain water-rights and environmental-flow review, flood-stage intake hydraulics, water-quality samples, receiving-capacity tests, and surveyed elevation and distance. The Ogallala transfer would require its own route and receiving tests.

Source: USGS daily discharge and quality flags. Applicable review: TCEQ Brazos environmental-flow rules and Brazos Watermaster.

Beta · flood peak timing screen

Harvey at Rosharon: when could an upstream intake change flow?

USGS approved 15-minute discharge and gauge-height readings let us compare Harvey's observed hydrograph with an idealized upstream diversion. The blue line assumes the entered rate was removed before the gauge with immediate effect, no return flow or added runoff. There is no selected intake or built conveyance. This is a flow screen, not a predicted flood level or damage result.

The flow floor and comparison threshold are user assumptions. Neither is a legal protected-flow value or a flood-stage threshold. The modeled removal is capped by both assumed intake capacity and observed flow above the floor.

Orange: observed discharge · Blue: assumed residual discharge · vertical scale: thousands of cfs. Gaps are not drawn across missing readings.

Observed peak at gauge

133,000 cfs

Aug 29, 4:30 PM CDT · recorded stage 52.65 ft

Idealized residual peak

132,000 cfs

Aug 29, 4:30 PM CDT · assumes removal before gauge

Flow removed in screen

24,157 AF

Arithmetic integral over observed 15-minute intervals; actual recoverable volume unknown

At the assumed 100,000 cfs comparison line, observed flow spent about 105.7 hours above it; the idealized residual spends about 100.0 hours. This is an illustrative flow metric, not hours of flooding. 406.75 of 408 event-window hours have adjacent valid discharge samples; 75 minutes across two gaps are excluded from integration.

What the gauge actually recorded above flood-stage markers

The recorded Harvey peak was 52.65 feet. Applying the NWS Rosharon (ROST2) stage markers as retrospective context gives the observed durations below. These are hours above a gauge-height marker, not hours any particular home was underwater. Current NWS markers are used for context; they do not reconstruct the 2017 warning record.

Flood stage · 43 ft

251.0 observed hours

Moderate stage · 47 ft

230.2 observed hours

Major stage · 51.3 ft

194.0 observed hours

No alternate stage or stage-category duration is calculated for the diversion scenario. Stage response requires a calibrated hydraulic model.

Evidence still needed for actual flood relief: an upstream intake location and travel time; sub-hourly hydraulics with cross sections, tributary inflows and backwater; a surveyed elevation datum and stage-to-inundation mapping; exposed buildings and assets; downstream safety checks. The recorded 52.65-foot gauge peak cannot be lowered by simply subtracting cfs from feet. The USGS Harvey inundation data show the historical extent, while the Lower Brazos hydraulic study provides a starting point for a calibrated project comparison. Neither dataset alone predicts a diversion's effect. USGS discharge readings · USGS gauge-height readings · Download observations and provenance.

Beta · upstream intake shortlist

Where should a floodwater intake be investigated first?

Choose the threatened reach. The table checks how much water passed each upstream USGS gauge before that reach's observed Harvey crest, using the same assumed rate cap and flow floor at every gauge. An upstream gauge is a measurement point, not an approved intake site. The named reach is a screening proxy; a real population and floodplain must be mapped before siting.

Target gauge 08114000 peaked at 122,000 cfs on Aug 31, 10:45 PM CDT. The table ends each source calculation at that timestamp. Gauges are ordered along the main stem; local tributary inflows and floodplain storage make their hydrographs different.

Upstream gaugeObserved gauge peakFirst screened flow before target crestScreened AF before crestSampled hours with flow above floor
Brazos River near HempsteadUSGS 08111500101,000 cfsAug 28, 5:00 PM CDTAug 27, 9:15 AM CDT8,723105.8585 min gaps excluded
Brazos River at San FelipeUSGS 08111850146,000 cfsAug 29, 1:15 AM CDTAug 27, 1:30 PM CDT8,570104.090 min gaps excluded

How to read this: the displayed acre-feet are independent arithmetic screens at different points on the same river. Do not add the rows. A larger number at a gauge does not identify a buildable intake or prove earlier flood relief: the water may arrive too late at the protected population, a tributary may add flooding downstream, and the removal may shift risk elsewhere. Stage, diversion rights, sediment, pump startup, pipe capacity, energy, land access and downstream environmental flows remain untested. The next engineering comparison must pair candidate parcels and threatened neighborhoods with a calibrated lower-Brazos hydraulic model.

Download the upstream USGS readings and source links

Beta · Harvey scale and response timing

How quickly would a flood diversion need to scale?

Harvey's seven-day rainfall over the five pilot watersheds totaled 8,377,874 acre-feet (8.38 million AF). That is rainfall over land, not water passing one intake or a full-storm total. The timeline below replays a separate 17-day USGS river record at Rosharon to compare no diversion with a system that starts when the observed gauge height crosses a selected trigger and ramps up over time.

Operating priority: warnings, evacuation and downstream safety first; test whether a selected intake measurably reduces flood exposure; then move eligible water to storage or demand along a route and to a receiving aquifer if it can accept it. The modeled capacity assumes a prebuilt, permitted system ready to operate. A forecast alone cannot build one.

Trigger height is a retrospective demonstration, not an operating rule. Flood stage at this gauge is 43 ft under current NWS markers. Earlier upstream warning and real-time forecast data would be needed for advance activation. The flow floor is an assumption, not an environmental-flow or water-right decision.

Observed triggerAug 27, 5:45 PM CDTRosharon stage reading
Idealized removal before crest14,050 AFAt the same gauge; flood damage reduction unknown
Removal over 17-day gauge window108,477 AFArithmetic ceiling; actual recovery unknown
Peak flow: observed → assumed133,000 → 128,000 cfsNo modeled stage or inundation change

Daily flow passing the gauge and idealized removal

Daily bins use UTC. Orange is observed gauge throughput; blue is the assumed amount removed from that same flow. These bars do not represent rainfall totals.

Aug 25
0 AF removed
Aug 26
0 AF removed
Aug 27
13 AF removed
Aug 28
5,462 AF removed
Aug 29
9,607 AF removed
Aug 30
9,711 AF removed
Aug 31
9,917 AF removed
Sep 1
9,917 AF removed
Sep 2
9,917 AF removed
Sep 3
9,917 AF removed
Sep 4
9,917 AF removed
Sep 5
9,917 AF removed
Sep 6
9,917 AF removed
Sep 7
9,917 AF removed
Sep 8
4,345 AF removed
Sep 9
0 AF removed
Sep 10
0 AF removed

Calculation: at each adjacent 15-minute sample, assumed removal is min(installed capacity × availability × elapsed ramp fraction, max(0, observed cfs − flow floor)). Trapezoids convert that rate to acre-feet. 406.75 hours of adjacent readings are included; 75 minutes of gaps are excluded. Removal is assumed to affect Rosharon immediately and perfectly; no travel delay, local runoff, backwater, treatment, losses, cost, power, receiving-site limit or operating outage beyond the entered availability is simulated. Observed and assumed flows are two scenarios for the same water, never additive. Actual life safety, flood-damage reduction, delivery and aquifer recharge require site-specific engineering and approvals.

NOAA rainfall ledger · USGS 15-minute observations · NOAA forecasts

Harvey retrospective · proposed corridor

What could a prebuilt route move?

This beta stress test applies hypothetical, continuous equipment to the observed 17-day Rosharon daily-flow record. The intermediate stop and Ogallala endpoint are unnamed planning placeholders, with no surveyed alignment or accepted receiving site. Enter route assumptions to see the scale of transport and energy. A forecast can trigger operations; it cannot create a corridor before landfall.

Decision order: protect people and avoid transferring risk downstream; test whether an intake lowers flood peaks and damage at the places that matter; then maximize movement of eligible excess water within intake, route, storage and receiving-site limits. This calculator has no flood-inundation or damage model, so its volume output is not a flood-safety result.

Source and allocation

The floor is illustrative, not a protected-flow determination or water right. Flow at one gauge is not storm-attributable or necessarily available to divert.

Two assumed route legs

The starting 350 + 350 km and 250 + 250 m are examples only. Velocity is a travel-time assumption, not a pipe design.

Gauge-side arithmetic ceiling23,802 AFAcross the observed 17 days
Allocated to intermediate stop4,760 AFFirst arrival after about 4.1 days
Allocated toward Ogallala19,041 AFFirst arrival after about 8.1 days
Elevation-only pump energy45 GWhAbout 156.2 MW at full intake
Forecast and startup: 72 hours of warning gives 3 days for readiness, but floodwater can be taken only when it actually reaches an authorized intake. A route assumed to start empty would first require about 14,463 AF inside its conduits at full rated flow and the entered velocity. This is a simple flow × travel-time proxy, not designed storage. First water reaches the intermediate stop about 4.1 days after intake and the distant endpoint about 8.1 days after intake; the endpoint total may arrive after the 17-day gauge window. A prefilled or staged system has different startup needs.

For an approaching storm, use official NOAA river forecasts for planning and update the modeled input as observations arrive. This page replays 2017 observations; it does not predict a future hurricane or issue an operating order.

Method and limits: Each day's screened rate is min(built cfs, max(0, daily mean cfs − assumed floor)). One cfs-day equals 1.98347 AF. Allocated volumes assume eventual passage and draining with no losses; they are not the amounts delivered by September 10. Pump energy uses ρgH × volume / efficiency for entered elevation lift only. Friction, surge protection, treatment, intermediate demand, reservoir operations, rights, actual route capacity, storage and recharge acceptance are absent. Daily mean flow cannot establish peak flood relief, life safety or damage avoided; those require time-resolved hydraulic and inundation analysis. No project cost or aquifer gain is inferred. USGS source and daily flags.

Harvey to Ogallala feasibility

Data needed for a defensible recovery calculation

The project now includes the observed rainfall, daily USGS river flows and the official High Plains aquifer boundary. Texas's current groundwater model and other public sources are identified below. Recovery is not yet calculable: an intake and recharge site must be chosen before legal availability, protected flows, water quality, route design and measured recharge capacity can be resolved. The recovery result is intentionally blank, not zero.

Required inputStatusUse and next step
Observed Harvey rainfall and watershed areasloadedGross precipitation context; not divertible runoff Download data Official source
Observed river flowloadedTotal daily gauge throughput; requires event baseline, routing and intake-specific analysis Download data Official source
High Plains aquifer extentloadedRegional extent only; does not show suitable injection or infiltration sites Download data Official source
Texas High Plains hydrogeology and groundwater availabilitysource identifiedRequires model package ingestion and extraction for a selected site; regional model is not a recharge permit Official source
Well levels and change in groundwater storagesource identifiedSelect current monitored wells near a proposed site and document measurement dates Official source
Existing surface-water rights and legal availabilitysite specific requiredTCEQ water-right authorizations and basin Water Availability Model at the exact proposed diversion Official source
Environmental flows and downstream obligationssite specific requiredApproved protected-flow schedule by diversion point and date Official source
Event-water and receiving-aquifer qualitysite specific requiredSample stormwater and local groundwater; treatment and compatibility review Official source
Intake, diversion and temporary-storage capacityengineering requiredSurveyed location, flood-stage operating limits, pump curve and hourly capacity
Conveyance route, elevation, energy and lossesengineering requiredSelect alignment, elevation profile, right-of-way, pipe/canal design, pump energy and transit losses Official source
Actual receiving-site recharge rate and storage responsefield test requiredGeology, infiltration or injection testing, mounding and groundwater-flow modeling at the actual site Official source
Permits, land access, capital and operating costsapproval requiredWritten authorizations, local district rules, landowner rights and priced design Official source
Download machine-readable data inventory

Method and checks

The NOAA observation band reports inches. All seven daily TIFFs matched the input pack’s SHA-256 hashes; the summed grid reproduced the project’s 54.264-inch grid maximum. Each USGS polygon was intersected with individual grid cells by fractional area, with area weighting in EPSG:5070. A cell counted only if all seven days had valid observations. HUC12 sums match parent HUC8 volume within one acre-foot after rounding; grid coverage is essentially complete.

The current WBD boundaries were queried September 25, 2026. Historic 2017 boundaries might differ. This independent project calculation still needs a separate hydrologist’s review before engineering use.

Source files and next gate

Official rainfall data: NOAA Stage IV . Official boundaries: USGS WBD map service . The download records each grid hash, period, method and every basin value. The next calculation is storm-attributable runoff from USGS hydrographs, followed by protected flow and intake feasibility.

Download full ledger (JSON)
Earlier independent HUC10 rainfall comparison

A university student analysis interpolated GHCN station totals over 12 named study areas. It is preliminary and uses a different grid, method and time window from this NOAA Stage IV ledger. Its table labels the period “10-day” while the text gives August 24–September 1; use it only as a comparison, never mix or sum the two datasets. Original paper

Study areaEstimated inches
West Fork San Jacinto River25.30
West Fork San Jacinto River-Conroe Lake19.33
Caney Creek-Lake Creek18.58
Crystal Creek-West Fork San Jacinto River22.83
Frontal Lake Houston30.55
Little Cypress Creek-Cypress Creek28.42
Walnut Creek-Spring Creek24.84
Peach Creek-Caney Creek22.06
Tarkington Bayou-Luce Bayou31.96
Winters Bayou-East Fork San Jacinto River24.37
East Fork San Jacinto River-Frontal Lake Houston27.23
Buffalo Bayou-San Jacinto River40.23
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