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.
Five pilot basins
Gross volumes are calculated from fractional raster-cell overlap. All five basins have 100% valid grid coverage to the displayed precision.
| HUC8 | Basin | Area (km²) | Mean rain (in.) | Gross rain (acre-ft) | HUC12s |
|---|---|---|---|---|---|
| 12040101 | West Fork San Jacinto | 2,801 | 22.39 | 1,291,806 | 25 |
| 12040102 | Spring | 1,960 | 29.21 | 1,179,015 | 20 |
| 12040103 | East Fork San Jacinto | 2,577 | 27.17 | 1,441,748 | 25 |
| 12040104 | Buffalo-San Jacinto | 3,063 | 36.15 | 2,279,764 | 28 |
| 12070104 | Lower Brazos | 4,255 | 24.94 | 2,185,541 | 41 |
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 +
| HUC12 | Name | Mean rain (in.) | Gross acre-ft | Coverage |
|---|---|---|---|---|
| 120401010101 | Rocky Creek-West Fork San Jacinto River | 20.72 | 63,435 | 100.00% |
| 120401010102 | McGary Creek | 20.87 | 28,604 | 100.00% |
| 120401010103 | West Sandy Creek | 20.63 | 47,227 | 100.00% |
| 120401010104 | Robinson Creek-West Fork San Jancinto River | 21.34 | 52,485 | 100.00% |
| 120401010201 | East Sandy Creek | 20.35 | 26,169 | 100.00% |
| 120401010202 | McDonald Creek-West Fork San Jacinto River | 20.95 | 63,465 | 100.00% |
| 120401010203 | Caney Creek | 19.27 | 41,557 | 100.00% |
| 120401010204 | Hostetter Creek-Lake Conroe | 20.44 | 66,624 | 100.00% |
| 120401010205 | Little Lake Creek-Lake Conroe | 20.01 | 52,592 | 100.00% |
| 120401010206 | Town Creek-Lake Conroe | 20.82 | 51,124 | 100.00% |
| 120401010207 | White Oak Creek-West Fork San Jacinto River | 22.88 | 44,379 | 100.00% |
| 120401010301 | Flagtail Creek-Lake Creek | 18.05 | 47,337 | 100.00% |
| 120401010302 | Garretts Creek | 18.28 | 30,514 | 100.00% |
| 120401010303 | Kidhaw Branch-Lake Creek | 20.08 | 39,297 | 100.00% |
| 120401010304 | Haynie Creek-Little Caney Creek | 19.90 | 38,679 | 100.00% |
| 120401010305 | Sand Creek-Caney Creek | 20.63 | 41,352 | 100.00% |
| 120401010306 | Town of Dobbin-Lake Creek | 22.36 | 34,028 | 100.00% |
| 120401010307 | Landrum Creek-Lake Creek | 23.24 | 65,360 | 100.00% |
| 120401010308 | Mound Creek-Lake Creek | 23.00 | 73,972 | 100.00% |
| 120401010401 | Stewarts Creek-West Fork San Jacinto River | 22.64 | 39,639 | 100.00% |
| 120401010402 | Little Caney Creek-West Fork San Jacinto River | 23.40 | 39,039 | 100.00% |
| 120401010403 | Crystal Creek | 21.36 | 54,924 | 100.00% |
| 120401010404 | Black Slough-West Fork San Jacinto River | 28.06 | 87,537 | 100.00% |
| 120401010501 | Bens Branch | 32.16 | 100,717 | 100.00% |
| 120401010502 | San Jacinto Dam | 35.06 | 61,750 | 100.00% |
Spring · 12040102 · 20 subwatersheds +
| HUC12 | Name | Mean rain (in.) | Gross acre-ft | Coverage |
|---|---|---|---|---|
| 120401020101 | Mound Creek-Cypress Creek | 29.90 | 71,813 | 100.00% |
| 120401020102 | Live Oak Creek | 29.23 | 29,363 | 100.00% |
| 120401020103 | Mallard Lake-Cypress Creek | 33.23 | 103,248 | 100.00% |
| 120401020104 | Dry Creek-Cypress Creek | 35.28 | 58,780 | 100.00% |
| 120401020105 | Little Cypress Creek | 32.10 | 92,642 | 100.00% |
| 120401020106 | Marshall Lake-Cypress Creek | 30.01 | 87,581 | 100.00% |
| 120401020107 | Turkey Creek-Cypress Creek | 31.40 | 93,737 | 100.00% |
| 120401020201 | Kickapoo Creek-Spring Creek | 28.07 | 51,531 | 100.00% |
| 120401020202 | Threemile Creek-Brushy Creek | 28.33 | 74,286 | 100.00% |
| 120401020203 | Birch Creek-Walnut Creek | 27.40 | 53,810 | 100.00% |
| 120401020204 | Mink Branch-Walnut Creek | 28.69 | 58,990 | 100.00% |
| 120401020205 | Sugar Creek-Spring Creek | 29.24 | 49,906 | 100.00% |
| 120401020206 | Hurricane Creek-Mill Creek | 25.14 | 35,023 | 100.00% |
| 120401020207 | Kachel Lake-Mill Creek | 26.16 | 25,982 | 100.00% |
| 120401020208 | Decker Branch-Mill Creek | 25.61 | 41,654 | 100.00% |
| 120401020209 | Dry Creek-Spring Creek | 25.21 | 53,927 | 100.00% |
| 120401020210 | Willow Creek | 28.05 | 82,388 | 100.00% |
| 120401020211 | Bear Branch-Panther Branch | 25.17 | 37,138 | 100.00% |
| 120401020212 | Panther Branch-Spring Creek | 26.82 | 41,968 | 100.00% |
| 120401020213 | Spring Creek | 32.51 | 35,249 | 100.00% |
East Fork San Jacinto · 12040103 · 25 subwatersheds +
| HUC12 | Name | Mean rain (in.) | Gross acre-ft | Coverage |
|---|---|---|---|---|
| 120401030101 | Hegar Branch-Caney Creek | 21.38 | 50,026 | 100.00% |
| 120401030102 | McRae Creek-Caney Creek | 22.05 | 56,860 | 100.00% |
| 120401030103 | West Fork Spring Branch-Spring Branch | 23.06 | 45,722 | 100.00% |
| 120401030104 | Cagle Branch-Caney Creek | 22.98 | 29,141 | 100.00% |
| 120401030105 | Dry Creek-Caney Creek | 26.13 | 43,106 | 100.00% |
| 120401030106 | Boggy Creek-Peach Creek | 23.48 | 59,933 | 100.00% |
| 120401030107 | Lawrence Creek-Peach Creek | 25.64 | 48,081 | 100.00% |
| 120401030108 | Jayhawker Creek | 27.40 | 33,788 | 100.00% |
| 120401030109 | Gully Branch-Peach Creek | 27.13 | 71,952 | 100.00% |
| 120401030110 | White Oak Creek | 28.86 | 49,238 | 100.00% |
| 120401030201 | Upper Tarkington Bayou | 28.42 | 84,140 | 100.00% |
| 120401030202 | Marsh Branch-Tarkington Bayou | 32.11 | 74,849 | 100.00% |
| 120401030203 | Lower Tarkington Bayou | 35.94 | 52,749 | 100.00% |
| 120401030204 | Indian Gulley-Luce Bayou | 41.49 | 88,192 | 100.00% |
| 120401030205 | Luce Bayou | 34.91 | 85,660 | 100.00% |
| 120401030301 | Boswell Creek | 24.59 | 30,975 | 100.00% |
| 120401030302 | Gourd Creek-Winters Bayou | 22.41 | 73,611 | 100.00% |
| 120401030303 | Hopkins Branch-Winters Bayou | 24.33 | 72,256 | 100.00% |
| 120401030304 | Nebletts Creek-Winters Bayou | 25.74 | 41,205 | 100.00% |
| 120401030305 | Cobb Creek-East Fork San Jacinto River | 24.90 | 63,547 | 100.00% |
| 120401030306 | McCombs Creek-East Fork San Jacinto River | 25.33 | 23,215 | 100.00% |
| 120401030307 | Miller Creek-East Fork San Jacinto River | 24.19 | 60,314 | 100.00% |
| 120401030308 | Oil Creek-East Fork San Jacinto | 25.06 | 43,456 | 100.00% |
| 120401030401 | Whiskey Branch-East Fork San Jancito River | 30.42 | 70,767 | 100.00% |
| 120401030402 | Orange Branch-East Fork San Jacinto River | 32.30 | 88,966 | 100.00% |
Buffalo-San Jacinto · 12040104 · 28 subwatersheds +
| HUC12 | Name | Mean rain (in.) | Gross acre-ft | Coverage |
|---|---|---|---|---|
| 120401040101 | Willow Fork | 32.56 | 66,845 | 100.00% |
| 120401040102 | Cane Island Branch | 34.76 | 29,474 | 100.00% |
| 120401040103 | Little Prong-Buffalo Bayou | 33.52 | 48,582 | 100.00% |
| 120401040104 | Barker Reservoir-Buffalo Bayou | 34.69 | 96,676 | 100.00% |
| 120401040201 | Langham Creek | 35.44 | 103,922 | 100.00% |
| 120401040202 | Bear Creek | 33.62 | 59,387 | 100.00% |
| 120401040203 | South Mayde Creek | 33.43 | 79,926 | 100.00% |
| 120401040301 | Jersey Lake-Whiteoak Bayou | 32.11 | 39,459 | 100.00% |
| 120401040302 | Cole Creek-Whiteoak Bayou | 33.55 | 92,060 | 100.00% |
| 120401040303 | Spring Branch-Buffalo Bayou | 34.48 | 96,204 | 100.00% |
| 120401040304 | Little Whiteoak Bayou-Whiteoak Bayou | 34.88 | 78,545 | 100.00% |
| 120401040305 | City of Houston-Buffalo Bayou | 34.26 | 37,251 | 100.00% |
| 120401040401 | Keegans Bayou-Brays Bayou | 35.12 | 179,626 | 100.00% |
| 120401040402 | Country Club Bayou-Brays Bayou | 35.43 | 86,687 | 100.00% |
| 120401040501 | Upper Sims Bayou | 34.79 | 85,070 | 100.00% |
| 120401040502 | Lower Sims Bayou | 40.36 | 107,001 | 100.00% |
| 120401040601 | Headwaters Greens Bayou | 32.63 | 58,337 | 100.00% |
| 120401040602 | Garners Bayou | 34.60 | 63,969 | 100.00% |
| 120401040603 | Upper Greens Bayou | 34.72 | 75,480 | 100.00% |
| 120401040604 | Halls Bayou | 37.48 | 103,849 | 100.00% |
| 120401040605 | Middle Greens Bayou | 38.40 | 38,158 | 100.00% |
| 120401040606 | Lower Greens Bayou | 40.55 | 62,951 | 100.00% |
| 120401040701 | Hunting Bayou | 40.84 | 88,893 | 100.00% |
| 120401040702 | Carpenters Bayou | 38.26 | 77,181 | 100.00% |
| 120401040703 | Vince Bayou-Buffalo Bayou | 41.60 | 132,178 | 100.00% |
| 120401040704 | Jackson Bayou-San Jacinto River | 37.84 | 112,068 | 100.00% |
| 120401040705 | Highlands Reservoir-San Jacinto River | 38.73 | 58,465 | 100.00% |
| 120401040706 | Goose Creek | 39.11 | 121,521 | 100.00% |
Lower Brazos · 12070104 · 41 subwatersheds +
| HUC12 | Name | Mean rain (in.) | Gross acre-ft | Coverage |
|---|---|---|---|---|
| 120701040101 | Headwaters Caney Creek | 17.32 | 31,769 | 100.00% |
| 120701040102 | Browning Branch-Brazos River | 16.43 | 17,668 | 100.00% |
| 120701040103 | Gibbs Creek-Caney Creek | 17.25 | 26,397 | 100.00% |
| 120701040104 | Ponds Creek-Clear Creek | 22.29 | 56,016 | 100.00% |
| 120701040105 | Threemile Creek-Clear Creek | 22.72 | 34,877 | 100.00% |
| 120701040106 | Lewisville Creek-Brazos River | 18.82 | 28,313 | 100.00% |
| 120701040107 | Dry Creek-Piney Creek | 21.42 | 44,975 | 100.00% |
| 120701040108 | Ives Creek-Brazos River | 21.28 | 50,098 | 100.00% |
| 120701040201 | Indian Creek-East Mill Creek | 22.50 | 47,919 | 100.00% |
| 120701040202 | Sandy Creek-East Mill Creek | 21.45 | 30,727 | 100.00% |
| 120701040203 | Jackson Creek-East Mill Creek | 20.35 | 40,395 | 100.00% |
| 120701040204 | East Mill Creek | 18.27 | 53,619 | 100.00% |
| 120701040205 | Upper West Mill Creek | 21.44 | 44,871 | 100.00% |
| 120701040206 | Middle West Mill Creek | 19.39 | 52,953 | 100.00% |
| 120701040207 | Post Oak Point Creek-Sandy Creek | 20.30 | 34,898 | 100.00% |
| 120701040208 | Lower West Mill Creek | 19.14 | 33,692 | 100.00% |
| 120701040209 | Sandy Creek-Mill Creek | 22.29 | 66,876 | 100.00% |
| 120701040210 | Deadman Creek-Mill Creek | 25.41 | 71,449 | 100.00% |
| 120701040301 | Harris Creek-Irons Creek | 25.86 | 42,860 | 100.00% |
| 120701040302 | Mulberry Creek-Irons Creek | 29.34 | 37,749 | 100.00% |
| 120701040303 | Dry Branch-Bessies Creek | 31.50 | 88,571 | 100.00% |
| 120701040304 | Bullinger Creek-Brazos River | 25.46 | 38,667 | 100.00% |
| 120701040305 | Upper Allens Creek | 20.70 | 37,642 | 100.00% |
| 120701040306 | Lower Allens Creek | 23.02 | 42,132 | 100.00% |
| 120701040307 | Cannons Lake-Brazos River | 28.01 | 46,008 | 100.00% |
| 120701040308 | Brookshire Creek-Bessies Creek | 31.41 | 77,322 | 100.00% |
| 120701040309 | Cottonwood Creek-Brazos River | 28.54 | 55,996 | 100.00% |
| 120701040401 | Sandy Branch-Brazos River | 29.42 | 96,144 | 100.00% |
| 120701040402 | Rabbs Bayou-Brazos River | 33.43 | 97,651 | 100.00% |
| 120701040403 | Steep Bank Creek-Brazos River | 36.77 | 58,076 | 100.00% |
| 120701040404 | Coon Creek-Cottonwood Creek | 28.91 | 48,205 | 100.00% |
| 120701040405 | Seabourne Creek-Big Creek | 29.01 | 56,603 | 100.00% |
| 120701040406 | Fairchilds Creek-Big Creek | 29.44 | 73,870 | 100.00% |
| 120701040407 | Worthington Lake-Big Creek | 30.53 | 55,850 | 100.00% |
| 120701040408 | Dry Creek-Rabbs Bayou | 31.29 | 68,012 | 100.00% |
| 120701040409 | Dry Bayou-Brazos River | 34.21 | 104,169 | 100.00% |
| 120701040501 | Cow Creek-Brazos River | 29.70 | 96,407 | 100.00% |
| 120701040502 | Varner Creek | 23.80 | 66,212 | 100.00% |
| 120701040503 | Harris Reservoir-Brazos River | 23.78 | 62,598 | 100.00% |
| 120701040504 | Middle Bayou-Brazos River | 17.70 | 17,682 | 100.00% |
| 120701040505 | Outlet Barzos River | 16.63 | 49,602 | 100.00% |
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 gauge | Days present | Reported river flow (acre-ft) | Estimated days |
|---|---|---|---|
| Brazos River near RosharonUSGS 08116650 | 17/17 | 2,210,638 | 0 |
| West Fork San Jacinto above Lake Houston near PorterUSGS 08068090 | 17/17 | 657,743 | 0 |
| Spring Creek near SpringUSGS 08068500 | 17/17 | 373,297 | 0 |
| East Fork San Jacinto near New CaneyUSGS 08070200 | 17/17 | 477,567 | 2 |
| Buffalo Bayou at HoustonUSGS 08074000 | 16/17 * | 423,709 | 3 |
* 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 flagsOne 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.
| Date (2017) | Observed daily mean (cfs) | Screened ceiling (acre-ft) |
|---|---|---|
| 2017-08-25 | 2,330 | 0 |
| 2017-08-26 | 17,800 | 0 |
| 2017-08-27 | 43,500 | 1,983 |
| 2017-08-28 | 71,600 | 1,983 |
| 2017-08-29 | 121,000 | 1,983 |
| 2017-08-30 | 117,000 | 1,983 |
| 2017-08-31 | 101,000 | 1,983 |
| 2017-09-01 | 101,000 | 1,983 |
| 2017-09-02 | 103,000 | 1,983 |
| 2017-09-03 | 98,100 | 1,983 |
| 2017-09-04 | 90,300 | 1,983 |
| 2017-09-05 | 78,200 | 1,983 |
| 2017-09-06 | 60,400 | 1,983 |
| 2017-09-07 | 44,500 | 1,983 |
| 2017-09-08 | 28,200 | 0 |
| 2017-09-09 | 20,200 | 0 |
| 2017-09-10 | 16,400 | 0 |
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 cfsAug 29, 4:30 PM CDT · recorded stage 52.65 ft
Idealized residual peak
132,000 cfsAug 29, 4:30 PM CDT · assumes removal before gauge
Flow removed in screen
24,157 AFArithmetic 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 hoursModerate stage · 47 ft
230.2 observed hoursMajor stage · 51.3 ft
194.0 observed hoursNo 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 gauge | Observed gauge peak | First screened flow before target crest | Screened AF before crest | Sampled hours with flow above floor |
|---|---|---|---|---|
| Brazos River near HempsteadUSGS 08111500 | 101,000 cfsAug 28, 5:00 PM CDT | Aug 27, 9:15 AM CDT | 8,723 | 105.8585 min gaps excluded |
| Brazos River at San FelipeUSGS 08111850 | 146,000 cfsAug 29, 1:15 AM CDT | Aug 27, 1:30 PM CDT | 8,570 | 104.090 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 linksBeta · 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.
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.
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.
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.
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 input | Status | Use and next step |
|---|---|---|
| Observed Harvey rainfall and watershed areas | loaded | Gross precipitation context; not divertible runoff Download data Official source |
| Observed river flow | loaded | Total daily gauge throughput; requires event baseline, routing and intake-specific analysis Download data Official source |
| High Plains aquifer extent | loaded | Regional extent only; does not show suitable injection or infiltration sites Download data Official source |
| Texas High Plains hydrogeology and groundwater availability | source identified | Requires model package ingestion and extraction for a selected site; regional model is not a recharge permit Official source |
| Well levels and change in groundwater storage | source identified | Select current monitored wells near a proposed site and document measurement dates Official source |
| Existing surface-water rights and legal availability | site specific required | TCEQ water-right authorizations and basin Water Availability Model at the exact proposed diversion Official source |
| Environmental flows and downstream obligations | site specific required | Approved protected-flow schedule by diversion point and date Official source |
| Event-water and receiving-aquifer quality | site specific required | Sample stormwater and local groundwater; treatment and compatibility review Official source |
| Intake, diversion and temporary-storage capacity | engineering required | Surveyed location, flood-stage operating limits, pump curve and hourly capacity |
| Conveyance route, elevation, energy and losses | engineering required | Select alignment, elevation profile, right-of-way, pipe/canal design, pump energy and transit losses Official source |
| Actual receiving-site recharge rate and storage response | field test required | Geology, infiltration or injection testing, mounding and groundwater-flow modeling at the actual site Official source |
| Permits, land access, capital and operating costs | approval required | Written authorizations, local district rules, landowner rights and priced design Official source |
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 area | Estimated inches |
|---|---|
| West Fork San Jacinto River | 25.30 |
| West Fork San Jacinto River-Conroe Lake | 19.33 |
| Caney Creek-Lake Creek | 18.58 |
| Crystal Creek-West Fork San Jacinto River | 22.83 |
| Frontal Lake Houston | 30.55 |
| Little Cypress Creek-Cypress Creek | 28.42 |
| Walnut Creek-Spring Creek | 24.84 |
| Peach Creek-Caney Creek | 22.06 |
| Tarkington Bayou-Luce Bayou | 31.96 |
| Winters Bayou-East Fork San Jacinto River | 24.37 |
| East Fork San Jacinto River-Frontal Lake Houston | 27.23 |
| Buffalo Bayou-San Jacinto River | 40.23 |