Bootstrap review report — d3_wd26_saguache_creek
Generated 2026-08-13 22:36 UTC for Division 3 / Water District 26.
This is a review checklist, not a finished config. Everything below is a suggestion from live DWR data — confirm or correct each section in config.yaml before running this basin for real.
1. Stream-name patterns
Assumed mainstem pattern: SAGUACHE CREEK (highest-count waterSource value). Candidates below by structure count — decide which are real tributaries worth their own centerline vs. noise, and add them to longitudinal.tributary_stream_patterns in priority order (more-specific names, e.g. "WEST FORK X", must precede substrings of themselves, e.g. "X").
| waterSource | structure count |
|---|---|
| SAGUACHE CREEK (assumed mainstem) | 86 |
| WERNER ARROYO | 18 |
| MIDDLE CREEK | 14 |
| JACKS CREEK (AKA SKELTON CREEK) | 13 |
| SHEEP CREEK | 12 |
| NORTH FORK SAGUACHE CREEK | 10 |
| FORD CREEK | 6 |
| BEAR CREEK | 5 |
| CROSS CREEK | 5 |
| HODDING CREEK | 3 |
2. Diversion / return classification
Auto-classified from structureType + name patterns: 176 diversions, 0 returns, 250 unclassified (neither pattern matched — these render as neither on the schematic unless added to return_flow_wdids/force_diversion_wdids or a type is added to the diversion/return type lists).
This layer needs the least manual work — it's the same heuristic the engine uses at runtime. Spot-check a sample rather than reviewing every row; if you have a water-year accounting spreadsheet for this basin, cross-reference it against the 'other' bucket specifically (that's where a real augmentation return with an unusual DWR structureType will hide).
2b. Cross-checked against decreed water rights (CDSS)
47 structure(s) have a decreed water right (CDSS waterrights/netamount) that disagrees with the structureType/name-pattern classification above. Same-agency evidence (DWR/HydroBase), not independent of DWR the way the NLDI topology check is — worth a glance, not an automatic correction.
| wdid | structure | currently | decreed uses suggest | decreed uses |
|---|---|---|---|---|
| 2605000 | W0001 WELL NO 01 | other | diversion | Irrigation |
| 2605001 | W1037 WELL NO 02 | other | diversion | Irrigation |
| 2605004 | W1745 WELL NO 03 | other | diversion | Irrigation, Stock |
| 2605005 | W1902 WELL NO HENSON 02 | other | diversion | Irrigation |
| 2605006 | W1902 WELL NO HENSON 04 | other | diversion | Irrigation |
| 2605012 | W3288 WEEKS WELL NO 01 | other | diversion | Irrigation |
| 2605013 | W3288 WEEKS WELL NO 02 | other | diversion | Irrigation |
| 2605014 | W3288 WEEKS WELL NO 03 | other | diversion | Irrigation |
| 2605015 | W0082 WELL NO 02 | other | diversion | Irrigation |
| 2605016 | 81CW135 WELL NO D 02A | other | diversion | Irrigation |
| 2605018 | 81CW135 WELL NO D 05A | other | diversion | Irrigation |
| 2605019 | W2276 WELL NO 01 | other | diversion | Irrigation |
| 2605020 | 81CW135 WELL NO D 07A | other | diversion | Irrigation |
| 2605021 | W0082 WELL NO 04 | other | diversion | Irrigation |
| 2605022 | 81CW168 WELL NO 04A | other | diversion | Irrigation |
| 2605023 | 81CW168 WELL NO 04AA | other | diversion | Irrigation |
| 2605029 | 83CW008 WELL NO 20R | other | diversion | Commercial, Domestic, Irrigation |
| 2605032 | 82CW075 WELL NO 02R | other | diversion | Irrigation |
| 2605035 | W2465 WELL NO 01 | other | diversion | Fishery, Irrigation, Wildlife |
| 2605040 | W1902 WELL NO S FARM 07 | other | diversion | Irrigation |
| 2605043 | W1902 WELL NO S FARM 15 | other | diversion | Irrigation |
| 2605044 | W1902 WELL NO S FARM 25 | other | diversion | Irrigation |
| 2605045 | W1902 WELL NO S FARM 01A | other | diversion | Irrigation |
| 2605046 | W1902 WELL NO S FARM 02A | other | diversion | Irrigation |
| 2605047 | W1902 WELL NO S FARM 06A | other | diversion | Irrigation |
| 2605048 | W1902 WELL NO S FARM 07A | other | diversion | Irrigation |
| 2605049 | W1902 WELL NO S FARM 08A | other | diversion | Irrigation |
| 2605050 | W1902 WELL NO S FARM 10A | other | diversion | Irrigation |
| 2605052 | W1902 WELL NO S FARM 25A | other | diversion | Irrigation |
| 2605053 | W0092 WELL NO 01 | other | diversion | Irrigation |
| 2605054 | W3679 WELL NO 01A | other | diversion | Irrigation |
| 2605055 | W0002 WELL NO 02 | other | diversion | Irrigation |
| 2605056 | 80CW046 WELL NO 30 | other | diversion | Irrigation |
| 2605057 | 80CW046 WELL NO 31 | other | diversion | Irrigation |
| 2605059 | 83CW0082 WELL NO 09 | other | diversion | Irrigation, Stock |
| 2605061 | W0030 WELL NO 01 | other | diversion | Irrigation |
| 2605062 | W0082 WELL NO 01 | other | diversion | Irrigation |
| 2605063 | W0082 WELL NO 03 | other | diversion | Irrigation |
| 2605098 | W0094 PUMP WELL NO 01 | other | diversion | Irrigation |
| 2605099 | W0094 PUMP WELL NO 03 | other | diversion | Irrigation |
| 2605100 | W0094 PUMP WELL NO 04 | other | diversion | Domestic, Irrigation, Stock |
| 2605101 | W0094 PUMP WELL NO 05 | other | diversion | Irrigation |
| 2605102 | W0094 PUMP WELL NO 06 | other | diversion | Irrigation |
| 2605103 | W0094 PUMP WELL NO 07 | other | diversion | Irrigation |
| 2605120 | W0207 WELL NO 01 | other | diversion | Irrigation |
| 2605121 | W0477 WELL NO 01 | other | diversion | Domestic, Municipal |
| 2605131 | W0533 WELL NO ART 01 | other | diversion | Irrigation |
3. Suspected nested tributaries
Still need a human decision — these tributary pairs are comparably close to EACH OTHER as to the mainstem — one may actually join the other rather than the mainstem directly (like Leavenworth Creek -> South Clear Creek in the Clear Creek basin). NLDI couldn't resolve these (no nearby flowline, or ambiguous/no downstream overlap within range) — if you know the real topology, set it in longitudinal.tributary_parent_overrides.
| tributary | possible parent | dist to possible parent (mi) | dist to mainstem (mi) | NLDI result |
|---|---|---|---|---|
| MIDDLE CREEK | JACKS CREEK (AKA SKELTON CREEK) | 0.38 | 0.84 | NLDI check failed: 429 Client Error: Too Many Requests for url: https://api.water.usgs.gov/nldi/linked-data/comid/position?f=json&coords=POINT%28-106.30971+38.171001%29 |
| JACKS CREEK (AKA SKELTON CREEK) | MIDDLE CREEK | 0.4 | 0.44 | NLDI check failed: 429 Client Error: Too Many Requests for url: https://api.water.usgs.gov/nldi/linked-data/comid/position?f=json&coords=POINT%28-106.300833+38.198217%29 |
| CROSS CREEK | JACKS CREEK (AKA SKELTON CREEK) | 0.28 | 1.23 | NLDI check failed: 429 Client Error: Too Many Requests for url: https://api.water.usgs.gov/nldi/linked-data/comid/position?f=json&coords=POINT%28-106.341788+38.186555%29 |
4. Gage placement risk
None — every gage with a resolvable position is within the placement cutoff.
5 more gage(s) pass but are within 2x the cutoff distance — worth a glance if the structure dataset changes later.
Next steps
- Fill in
tributary_stream_patternsfrom section 1. - Resolve section 3's flags (or confirm none apply).
- Resolve section 4's at-risk gages.
- Cross-reference
return_flow_wdids/force_diversion_wdidsagainst any local accounting source you have for this basin. - Review the rendered schematic for this district before relying on it.
Evolution of the network
Computed 2026-08-20 08:52 from 6 gage(s) with cached period-of-record data. Statistical tests (Mann-Kendall trend, Pettitt changepoint) require at least 8 years spanning at least 10 years of record -- gages below that report no signal, not "no change."
Data provenance & quality
Where these numbers come from and how far they can be trusted. Grade C (3/6 points) — the components below are the finding; the letter alone is not. Sources: DWR HydroBase snapshot HydroBase_CO_20260707 (imported 2026-08-19) for history, plus the CDSS REST API for current conditions.
| Check | State | What was measured |
|---|---|---|
| gage freshness | stale | newest gage reading is 45 day(s) old (target 7) |
| diversion record | expected-lag | newest diversion record is 293 day(s) old (DWR publishes ~1 year in arrears) |
| structure coverage | sparse | 11% of schematic structures have data |
Independent check: PASS — 100.0000% agreement across 162,753 stored values re-checked against DWR's authoritative record (HydroBase_CO_20260707), over 20 structures. 0 disagreement(s) beyond a 0.01 cfs tolerance. Checked 2026-08-19; a rotating sample covers the whole basin across successive runs, and the structures this report cites are checked every time.
Federal cross-check: PASS — 99.98% day-level agreement with USGS's own published records for the same gages, across 2 co-listed station(s) and 36,622 overlapping days (within max(2%, 0.5 cfs) daily). Pre-1950 records at some gages carry known between-agency day-stamp and transcription differences — scored at each year's best ±1-day alignment; residual disagreement is real historical divergence, flagged for review.
6 gage(s) / 70,934 daily values (1910-08-01–2026-07-06); 208 structure(s) with diversion records; 1548 with decreed rights. Methodology has not yet had independent expert review — treat every figure as an advisory screen, not an administrative or legal conclusion.
Read this first: the measurement network itself evolved
This basin was not always measured the way it is today — the API-era record is dense and recent, the early record sparse. 5 gage(s) and 91 structure(s) report in 2026, but structure reporting only reached half its modern level around ~1984. Every historical claim below is checked against this: long-term shifts that co-move with the growth of the network carry an explicit measurement-evolution caution, and abandonment screens whose idleness begins before the modern reporting era are flagged †.
| Decade | Gages with data (median yr) | Structures reporting (median yr) |
|---|---|---|
| 1910s | 1 | 0 |
| 1920s | 1 | 0 |
| 1930s | 1 | 0 |
| 1940s | 1 | 0 |
| 1950s | 2 | 32 |
| 1960s | 2 | 56 |
| 1970s | 2 | 62 |
| 1980s | 3 | 73 |
| 1990s | 2 | 72 |
| 2000s | 2 | 128 |
| 2010s | 2 | 145 |
| 2020s | 3 | 95 |
Gage flow trend & changepoints
Every located gage with a period of record — dot size scales with the strength of its flow trend (|Sen slope| in %/decade, the same statistic as the table below), color with direction. An amber ring marks a detected Pettitt changepoint. Click a gage to chart its trend and shift.
| Gage | Trend | Change / decade | Significance | Years | Changepoint |
|---|---|---|---|---|---|
|
▸
SAGUACHE CREEK NEAR SAGUACHE, CO SAGSAGCO |
↓ decreasing | -3.7% | p=0.000 | 115 | ~1949 |
5 other gage(s) show no significant trend or changepoint (not shown).
Mass-balance (network closure) trend
Structure divrec-history backfill coverage as of the last check: 11% of 652 schematic-relevant structures. 0 year(s) clear the 30% coverage gate so far -- the trend activates automatically once qualifying years span a full decade. No action needed; the nightly backfill keeps extending the record.
Reach gain/loss shifts (1950–2026)
Mass-balance kinks computed for every summer month back to 1950 (360 reach-snapshots) — which reaches gain or lose water, and how that has shifted across decades. Each shift is cross-checked against the observation record above: as more diversions became metered, "unaccounted" water shrinks mechanically, which can masquerade as a hydrologic shift.
No reach shows a statistically significant long-term gain/loss shift.
Groundwater now has its own tab: 100 monitored well(s), water-table trends, stream corridors, and the advisory depletion screen.
Reservoirs now has its own tab: 1 reservoir(s), end-of-year storage back to 1974, click-to-chart histories.
Cross-gage pattern fingerprint
Not enough gages with a long enough common-coverage window yet to fingerprint shared patterns.
The basin's aquifer story, from 11,966 water-level measurements across 100 monitored well(s) (39 alluvial, 25 bedrock, rest unclassified) — plus 1 administered well(s) reporting metered pumping through diversion records. Observation wells and pumping wells are different populations and are never conflated. Click a well to chart its record.
Well map
Every monitored well with a location — hover for identity, click to chart its water-level record below. ● alluvial ● bedrock / confined (Denver Basin, High Plains, etc. — one-way, no human-timescale recharge) ● unclassified — marker size scales with the strength of the well's water-level trend (|Sen slope| in ft/decade — the same Mann-Kendall/Sen statistic as the trends table below); the smallest, faintest dots have too little record to test.
3D aquifer x-ray
Every aquifer unit as its own 3D head surface — alluvial water table on top, Denver Basin members (Dawson, Denver, Arapahoe, Laramie–Fox Hills) stacked beneath where measured — interpolated from measured water levels and animated through time. Units are never mixed; surfaces exist only inside each unit's well coverage (no extrapolation); thin epochs are suppressed with their reason shown. Vertical scale exaggerated for readability; z is head elevation in feet. Advisory — measured heads, not a calibrated model.
Water-table trends
Of 38 well(s) with enough record for a trend test: 28 declining, 2 rising.
| Fastest-declining wells | Setting | ft / decade | Span | p |
|---|---|---|---|---|
| ▸ NA04201017AAC1 EW-57U | unknown | -5.53 | 23 yr | 0.0 |
| ▸ NA04201017ADC EW-78C | alluvial | -4.86 | 26 yr | 0.0 |
| ▸ NA04201017AAC2 EW-57C | alluvial | -4.0 | 11 yr | 0.0 |
| ▸ NA04300726ADC | unknown | -3.51 | 19 yr | 0.0005 |
| ▸ NA04201007CCC RG18 | alluvial | -2.78 | 57 yr | 0.0 |
| ▸ NA04300925DDD1 EW-61U | alluvial | -2.71 | 11 yr | 0.0112 |
| ▸ NA04300925DDD2 EW-61C | alluvial | -2.42 | 11 yr | 0.0236 |
| ▸ NA04300815CBB SAG 13 | unknown | -2.23 | 52 yr | 0.0012 |
Wells labeled by administrative world before anything else is said about them: tributary alluvium participates in the priority system; designated-basin and Denver Basin bedrock aquifers are governed differently and are excluded from stream-connection reasoning. Read bedrock declines differently too: deep bedrock aquifers recharge negligibly on human timescales, so a falling bedrock level is storage mining — effectively permanent — not a drought response that a wet year undoes. All screens advisory.
1 reservoir(s) with 1 storage measurement(s), 1974–1974. Basin storage as of 1973-11-01 (the record's own end — reservoir records publish ~annually): 250 AF across 1 reservoir(s). Storage change is real water the mass balance must credit — a losing reach beside a filling reservoir isn't losing water, it's banking it.
Reservoir map — how full is each vessel?
Each reservoir drawn as a vessel: bubble size ∝ its record-high storage, fill level = last recorded storage as a share of its surveyed capacity (USACE National Inventory of Dams) where a confident NID match exists — the tooltip names the matched dam — and of its own record high otherwise (a wrong capacity would be worse than an honest record high, so only confident joins upgrade). Hover for numbers, click to chart its history below the map. A dashed teal ring marks reservoirs reporting live DWR telemetry — their fill reflects yesterday's storage, drawn as a dotted tail on charts and treated as provisional until the next verified HydroBase snapshot supersedes it. ● <25% ● 25–60% ● 60–90% ● >90%
Basin storage, end of each water year
End-of-water-year totals; per-year reservoir counts shown because reporting coverage varies -- a total is only comparable to years with similar counts.
Largest reservoirs on record
Click a reservoir to chart its full storage history.
| Reservoir | Last recorded storage (AF) | As of |
|---|---|---|
| ▸ SAGUACHE RESERVOIR (2603581) | 250 | 1973-11-01 |
Decrees, seniority, and administrative calls connected to this basin's flow network. Advisory reading aids on public DWR data — not administrative or legal conclusions. Rights on file: 1690 across 1548 structure(s); 119 structure(s) carry 0 court-case references.
Abandonment radar (23 screens)
Absolute rights with 10+ years of no recorded diversions. Screens only — storage, alternate points, and plan operations can explain nonuse lawfully. And diversion REPORTING itself only reached its modern level ~1984 — idleness that begins before then may be unreported use, not nonuse (flagged † below).
- WM M STOWE D (2600696) (1876-06-01, 11.6 cfs decreed): last active 1957 — 68 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1984) -- early absence of record is weak evidence of nonuse
- SCHALLER D 2 (2600665) (1877-06-01, 1.0 cfs decreed): last active 1962 — 63 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1984) -- early absence of record is weak evidence of nonuse
- HODGSON D 1 (2600565) (1876-11-01, 1.6 cfs decreed): last active 1965 — 60 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1984) -- early absence of record is weak evidence of nonuse
- DAVEY HAGAN OVERFLOW D (2600521) (1911-12-31, 3.6 cfs decreed): last active 1973 — 52 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1984) -- early absence of record is weak evidence of nonuse
- HARENCE D 2 (2600552) (1886-04-01, 2.0 cfs decreed): last active 1973 — 52 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1984) -- early absence of record is weak evidence of nonuse
- JONES BENJAMIN D 2 (2600577) (1877-06-01, 1.0 cfs decreed): last active 1973 — 52 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1984) -- early absence of record is weak evidence of nonuse
- MEANS D (2600597) (1883-12-25, 16.0 cfs decreed): last active 1973 — 52 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1984) -- early absence of record is weak evidence of nonuse
- DAVEY RUSSELL SEEPAGE DR (2600522) (1872-05-01, 5.0 cfs decreed): last active 1975 — 50 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1984) -- early absence of record is weak evidence of nonuse
- DAVEY S,D&OVFL D 1,NO BR (2600523) (1872-05-01, 3.0 cfs decreed): last active 1975 — 50 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1984) -- early absence of record is weak evidence of nonuse
- DAVEY S,D&OVFL D 2 (2600524) (1872-05-01, 6.0 cfs decreed): last active 1975 — 50 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1984) -- early absence of record is weak evidence of nonuse
Compliance screens (131 advisory flags)
Screened 175 of 1548 structures with rights (182 have diversion history on file). A flag is a lead for expert review — augmentation plans, exchanges, and free-river conditions can make over-decree diversions lawful and are deliberately not modeled.
- MEANS D (2600597): Observed p99 daily rate 125.0 cfs (max 125.0) exceeds total decreed absolute 16.0 cfs across 814 recorded day(s).
- OKLAHOMA CO D (2600621): Observed p99 daily rate 100.0 cfs (max 150.0) exceeds total decreed absolute 6.6 cfs across 12838 recorded day(s).
- JONES BENJAMIN D 2 (2600577): Observed p99 daily rate 50.0 cfs (max 75.0) exceeds total decreed absolute 1.0 cfs across 1218 recorded day(s).
- SOUTH 38 D (2600676): Observed p99 daily rate 35.2 cfs (max 35.2) exceeds total decreed absolute 35.2 cfs across 2004 recorded day(s).
- LUENGEN D (2600588): Observed p99 daily rate 30.0 cfs (max 30.0) exceeds total decreed absolute 9.6 cfs across 1454 recorded day(s).
- WERNER B D (2600694): Observed p99 daily rate 30.0 cfs (max 40.0) exceeds total decreed absolute 6.3 cfs across 3906 recorded day(s).
- STAR D (2600677): Observed p99 daily rate 22.0 cfs (max 24.0) exceeds total decreed absolute 12.7 cfs across 27742 recorded day(s).
- HARTMAN BROS D 3 (2600555): Observed p99 daily rate 21.0 cfs (max 21.0) exceeds total decreed absolute 7.4 cfs across 630 recorded day(s).
- MOSES GOFF D 2 (2600611): Observed p99 daily rate 20.0 cfs (max 20.0) exceeds total decreed absolute 1.6 cfs across 11483 recorded day(s).
- GEORGE BALL D (2600545): Observed p99 daily rate 18.2 cfs (max 30.0) exceeds total decreed absolute 6.0 cfs across 9563 recorded day(s).
Seniority (top structures by decreed rate)
| Structure | Senior priority date | Rights | Decreed abs (cfs) | Decreed abs (AF) | Conditional? |
|---|---|---|---|---|---|
| USFS QP49D (2601133) | 1905-06-13 | 1 | 311.2 | 0 | — |
| USFS QP47G (2601125) | 1905-06-13 | 1 | 111.6 | 0 | — |
| USFS QP47B (2601120) | 1905-06-13 | 1 | 96.8 | 0 | — |
| USFS QP47H (2601126) | 1905-06-13 | 1 | 58.6 | 0 | — |
| USFS QP49M (2601142) | 1905-06-13 | 1 | 57.8 | 0 | — |
| USFS QP51M (2601155) | 1905-06-13 | 1 | 52.4 | 0 | — |
| LAGARITA D (2600581) | 1919-05-01 | 2 | 52.0 | 0 | — |
| USFS QP47J (2601127) | 1905-06-13 | 1 | 46.6 | 0 | — |
| USFS QP51C (2601146) | 1905-06-13 | 1 | 43.2 | 0 | — |
| USFS QP51D (2601147) | 1905-06-13 | 1 | 43.2 | 0 | — |
| ALEXANDER OVERFLOW D (2600829) | 1985-05-03 | 1 | 40.0 | 0 | — |
| USFS QP49E (2601134) | 1905-06-13 | 1 | 36.0 | 0 | — |
| USFS QP49G2 (2601137) | 1905-06-13 | 1 | 35.4 | 0 | — |
| SOUTH 38 D (2600676) | 1874-03-01 | 10 | 35.2 | 0 | — |
| USFS QP47F (2601124) | 1905-06-13 | 1 | 33.6 | 0 | — |
No inventory or legal-document changes detected since the daily watch began.
If a call were placed at a given seniority, which structures in this basin would be out of priority, and how much of their decreed rate would be curtailed? Computed from this basin's cached decrees.
What this does and doesn't model. Seniority arithmetic only: every right junior to the call is treated as curtailed. It does not model reach applicability — structures downstream of the calling point are not administered by it — and it applies no futile-call judgment. Read it as “who is junior to this date, and by how much,” not as a prediction of what the Division Engineer would actually order.
Pick a calling right
Real decrees from this basin, ordered by administration number — that is, by actual seniority. The years will look out of order, and that is correct: an administration number encodes the adjudication date as well as the appropriation date, so a right appropriated in 1970 can be administered ahead of one from 1950. A senior call curtails almost everything; a junior one curtails almost nothing.
Or enter an administration number directly
DWR administration numbers encode appropriation and adjudication dates; lower is more senior.