Upper Uncompahgre River

Evolution of the network

Source Our computation, no independent reference · computed here from the screened DWR record Source Our computation, no independent reference · no independent reference; see /methods

This year, in context

In the weeks around 2026-07-06 (the newest reading on file), flows at the 6 ranked gages are running at a median 21% of their own long-term norm for this window — 6 below a typical year, 0 at or above. Driest relative to its record: DALLAS CREEK NEAR RIDGWAY, CO, ranking 2nd lowest of 69 years.

Gage flow trend & changepoints

Of the 6 gages with enough record, 1 is trending down and 0 up, and 1 carries a detected shift. The clearest is Uncompahgre River at Colona, its annual mean flow changing -7.38 cfs per decade (-3.0% of its median annual flow) over 113 years (p=0.0067). The other 5 show no clear signal either way.

5 other gage(s) show no significant trend or changepoint (not shown).

How the measurement network itself changed

This basin was not always measured the way it is today — the API-era record is dense and recent, the early record sparse. 6 gage(s) and 178 structure(s) report in 2026, but structure reporting only reached half its modern level around ~1970. 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 †.

Mass-balance (network closure) trend

Structure divrec-history backfill coverage as of the last check: 11% of 1547 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 (1956–2026)

Mass-balance kinks computed for every summer month back to 1956 (816 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.

• UNCOMPAHGRE RIVER AT COLONA, CO.: reach shifted from +432 cfs to +41 cfs summer mean (more losing, p=0.000, 71 yr) [alluvial valley: real alluvial aquifer -- a decades-long shift toward losing is the classic signature of alluvial pumping and urbanization] [measurement-evolution caution: this shift co-moves with the growth of the gage/metering network (rho=-0.57) -- part of it may be unaccounted water becoming accounted, not hydrologic change]
• UNCOMPAHGRE RIVER BELOW RIDGWAY RESERVOIR, CO: reach shifted from +300 cfs to +202 cfs summer mean (more losing, p=0.044, 38 yr) [sedimentary plains/foothills: moderate groundwater connectivity -- gain/loss shifts can be real aquifer response; corroborate with nearby well records]
• UNCOMPAHGRE RIVER NEAR RIDGWAY, CO.: reach shifted from +62 cfs to +27 cfs summer mean (more losing, p=0.028, 26 yr) [alluvial valley: real alluvial aquifer -- a decades-long shift toward losing is the classic signature of alluvial pumping and urbanization]

Groundwater now has its own tab: 10 monitored well(s), water-table trends, stream corridors, and the advisory depletion screen.

Reservoirs now has its own tab: 11 reservoir(s), end-of-year storage back to 1974, click-to-chart histories.

Cross-gage pattern fingerprint

Over the 26-year window with full coverage (2001–2026), the dominant shared pattern across 3 gage(s) explains 88% of year-to-year variance (almost certainly a basin-wide climate/snowpack driver).

All gages in this window move with the shared pattern -- no localized outlier.

Structures most implicated by reconciliation (as of 2026-07-06)

Which structures' data absorbed the most correction when the current mass-balance snapshot was reconciled -- see the Historical tab for the full picture on any date.

• DAVE WOOD SPRING (return): +2.4 cfs (3% of that reach's correction)
• FAIRWAY PINES ESTATE OWNERS POND 1 (diversion): +2.4 cfs (3% of that reach's correction)
• FAIRWAY PINES ESTATE OWNERS POND 2 (diversion): +2.4 cfs (3% of that reach's correction)
• MCKENZIE CANAL (diversion): +2.4 cfs (3% of that reach's correction)
• HIGHLINE DITCH (diversion): +2.4 cfs (3% of that reach's correction)
• SHORTLINE DITCH (diversion): +2.4 cfs (3% of that reach's correction)
• JOSSI SPRING PIPELINE (return): +2.4 cfs (3% of that reach's correction)
• ERGEN SPRING #2 (return): +2.4 cfs (3% of that reach's correction)
• ERGEN SPRING #3 (return): +2.4 cfs (3% of that reach's correction)
• CALL DITCH (diversion): +2.4 cfs (3% of that reach's correction)

Source DWR administrative record · verify at DWR groundwater wells ↗ Source DWR administrative record · verify at DWR well permits ↗

23 water-level measurements across 10 monitored well(s) — 7 alluvial, 1 bedrock — plus 3 administered well(s) reporting metered pumping.

Well map

3D aquifer x-ray

Every aquifer unit as its own head surface, animated through time.

Water-table trends

Of 0 well(s) with enough record for a trend test: 0 declining, 0 rising.

Stream corridors — the surface connection

Where a reach's gain or loss has shifted, the wells within two miles of its anchoring gage and what their water table did over the same era.

UNCOMPAHGRE RIVER NEAR RIDGWAY, CO.: 2 alluvial well(s) nearby

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.

Source DWR administrative record · verify at DWR structure records ↗

11 reservoir(s) with 2,090 storage measurement(s), 1974–2026. Basin storage as of 2025-10-31 (the record's own end — reservoir records publish ~annually): 66,111 AF across 1 reservoir(s).

Reservoir map — how full is each vessel?

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 row to chart its full storage history, or open its dossier for rights, documents and dam-safety facts.

Source Independent agency measurement · fetched 2026-09-12 · verify at NRCS report generator ↗ Source Our computation, scored against a reference · NRCS forecast, graded here against the gage record

Snow-water equivalent, WY2026

A trace of snow at 1 of 1 sites (0.1 in of water at most); the median for the date is zero, so there is no percent to show yet. The snow year begins in October. The chart shows the full water year just ending.

NRCS SNOTEL, daily. Sites are assigned to the district whose boundary contains them — the snow that feeds this district can also sit in a neighboring headwater district.

Two ways a snow year goes wrong (1981–2026)

A bad snow year here comes in two flavors (both called snow droughtA winter that shorts the snowpack. It happens two ways: a dry one, where the snow never comes, and a warm one, where near-normal snow falls but melts off weeks early -- and the river feels them differently.), and the river feels them differently. In 10 of the last 46 winters the snow never came — the pack peaked below 80% of its median. In 1 more, the snow came but left early — a near-normal peak melted out two weeks or more ahead of its usual date, sending the water down before the season needed it. This year was one of the dry ones: the pack peaked at 48% of median.

The snow never came: 1981, 1988, 1990, 2001, 2002, 2007, 2012, 2013, 2018, 2026. The snow left early: 1989.

Computed by this site from 1 SNOTEL site’ full daily records (NRCS AWDB, back to 1981). Each year is measured against each site’s own multi-decade median — not the 1991–2020 normal the chart above uses — so the 1980s grade against a fair baseline. Peak and melt-out need 85% of the season’s days on the record; thin years are dropped, not guessed. Derived from snow measurements alone — it cannot tell dry-from-warm causes apart, only what the snowpack did.

Runoff outlook — Ridgway Reservoir Inflow

NRCS's final issue (2026-06-01) calls it even odds that at least 14 kAF arrives over 06-01 to 07-31 — 22% of a normal season; almost certainly at least 6, probably not more than 22. Our own record at this gage shows 9 kAF actually delivered (partial record: 35 of 61 days). New forecasts begin in January. How to read these numbers →

How good are these forecasts here? (1993–2025)

Grading every April issue against what the river then delivered, measured at this gage’s own record — 32 seasons: the median miss of the 50% forecast is 21%, with a high bias of 11%, and the observed volume landed inside the stated 10–90% band 69% of the time (a calibrated forecast would say 80%).

Computed by this site: NRCS's archived April issues (their period as issued each year) against the observed volume in DWR’s published record; years with under 90% daily coverage are dropped, not summed. A grade of the forecast, never of the forecasters — these are hard rivers. How this point ranks among every graded Colorado forecast point →

What April snow has meant for this river (1989–2025)

Across 37 measured years, the season’s water has closely followed the April snowpack: a year opening April with 80% of median snow has typically gone on to deliver about 81% of a normal season (a snow-to-runoff elasticityHow strongly one number moves with another. A snow-to-runoff elasticity of 1.5 means a 10% shortfall in April snowpack has typically become a 15% shortfall in the season's water. of 0.8). In warm, early-melt years the river delivered a median of 51% of a normal season, against 112% in typical years — the timing of the melt matters, not just its size.

Computed by this site: the district’s April 1 SWE (% of each SNOTEL site’s own-record median) against the observed April–July volume at this gage (% of its median season) — a fixed window every year, unlike the forecast grades above, which use each issue’s own period. The slope is fit so single wild years can’t steer it (Theil–Sen, log space); years missing 10% of their days are dropped.

Runoff outlook — Uncompahgre R at Colona

NRCS's final issue (2026-06-01) calls it even odds that at least 12 kAF arrives over 06-01 to 07-31 — 16% of a normal season; almost certainly at least 7, probably not more than 24. Our own record at this gage shows 5 kAF actually delivered (partial record: 36 of 61 days). New forecasts begin in January. How to read these numbers →

How good are these forecasts here? (1950–2025)

Grading every April issue against what the river then delivered, measured at this gage’s own record — 75 seasons: the median miss of the 50% forecast is 24%, with a high bias of 7%, and the observed volume landed inside the stated 10–90% band 78% of the time (a calibrated forecast would say 80%).

Computed by this site: NRCS's archived April issues (their period as issued each year) against the observed volume in DWR’s published record; years with under 90% daily coverage are dropped, not summed. A grade of the forecast, never of the forecasters — these are hard rivers. How this point ranks among every graded Colorado forecast point →

What April snow has meant for this river (1981–2025)

Across 45 measured years, the season’s water has closely followed the April snowpack: a year opening April with 80% of median snow has typically gone on to deliver about 60% of a normal season (a snow-to-runoff elasticityHow strongly one number moves with another. A snow-to-runoff elasticity of 1.5 means a 10% shortfall in April snowpack has typically become a 15% shortfall in the season's water. of 1.3). In warm, early-melt years the river delivered a median of 38% of a normal season, against 100% in typical years — the timing of the melt matters, not just its size.

Computed by this site: the district’s April 1 SWE (% of each SNOTEL site’s own-record median) against the observed April–July volume at this gage (% of its median season) — a fixed window every year, unlike the forecast grades above, which use each issue’s own period. The slope is fit so single wild years can’t steer it (Theil–Sen, log space); years missing 10% of their days are dropped.

Source Our computation, no independent reference · computed here from the screened DWR record Source Independent agency measurement · fetched 2026-09-08 · verify at U.S. Drought Monitor ↗

Right now

This is the 3rd-driest week 27 in 114 years of record at UNCOMPAHGRE RIVER AT COLONA, CO. (as of 2026-06-29; this week’s flow sits at the 3rd percentileRank against the record: a river at its 5th percentile is lower than it was in 95 of the past 100 years on this same date. for the date). On this week’s US Drought Monitor, San Juan County is 6% in D3 extreme drought (2026-09-08). The law agrees: the most senior active call leaves 25% of this district’s decreed flow rights junior to the calling right this week.

Every year since 1912, week by week

Each thin row is a year at UNCOMPAHGRE RIVER AT COLONA, CO.; each cell is one week’s flow ranked against the same calendar week of every other year — warm means dry for the date, blue wet, so seasonality cancels and droughts appear as warm bands. Gaps are missing record, never a dry river. Click a year to reconstruct it on the Historical tab.

This year against its analogs

Over the 26 weeks recorded so far, 2026’s weekly trace most resembles 2021 (mean gap 7.2 percentile points; next closest 2013 (8.1), 2002 (8.5)). The analog’s remainder is drawn as context — its ending is what happened to it, not a forecast for this year.

The Drought Monitor’s view since 2000

Mean share of area in each class across Ouray, San Juan counties — the counties this district’s gages sit in, which overlap the district imperfectly. The Drought Monitor weighs soils, vegetation and local reports; it is CONTEXT beside the river’s own record above, not the water-rights picture.

The law’s own drought gauge

When water runs short, administration answers: calls reach further back in time, and more decreed rights go junior to the calling right. This is that response, weekly since 2003 — the share of this district’s decreed flow rights junior to the most senior active call. Watch it spike in the named droughts below, and linger after the river recovers.

Computed from DWR’s call record (35 calls touching this district) against the district’s rights index. Scoping is deliberately coarse — a call’s own district, or districts named in its comments — and this is administration’s RESPONSE, not a per-structure verdict (each dossier’s curtailment card does that, with stream miles). A deepening call can also reflect growing demand, not only shrinking supply.

This basin’s droughts, by its own record

Detected mechanically: the 26-week smoothed percentile below the 30th for at least 20 weeks; recovered on regaining the 50th. The water-table clock compares each monitoring well against its own pre-drought median (the 3 years before onset) and dates the year the median well got back — the aquifer remembers longest, and “still below” is a finding, not a gap. The knobs are stated because the episode list depends on them — a different reasonable choice merges or splits episodes at the edges. Names are attached where an episode overlaps a drought Colorado already talks about.

When this basin claimed its water

Every bar is a year’s new appropriations (1,039 rights across 115 years of shared record), colored by that year’s wetness from the barcode above. Here the correlation is -0.01 — essentially no wet-dry pattern; here, law and settlement set the pace, not the weather. Across the state both behaviors exist: ephemeral southwest basins file after wet demonstrations, transbasin-source basins under drought — and the biggest statewide filing waves sat in the 1950s drought and after 2002, not in the wet 1980s–90s.

Appropriation dates are the CLAIMED initiation of a right, not the courthouse filing date; the record is survivor-biased (abandoned claims are absent, so failed dry-era scrambles are undercounted); and the big 1960s and 2000s spikes sit on legal events — the pre-1969-Act adjudication era and 2000s legislation — not on weather. A correlation here is a description, never a cause.

New to how a dry winter becomes a call on the river? Anatomy of a drought walks the chain in four minutes — snow to rivers to reservoirs to calls to the water table.

Who serves it, who protects it

Two registers the site fetches on their own schedules, read for this district. Neither is a DWR record; each links its own page and its agency.

Public water systems here

Source Register of another agency · fetched 2026-09-08 · verify at EPA SDWIS ↗

5 systems touch this district (5 community systems reporting 3,869 people served, a figure that counts a wholesaler's customers twice); none carries an open health-based violation on EPA's record.

Instream-flow rights held by the state

Source Register of another agency · fetched 2026-09-08 · verify at CWCB instream flow program ↗

15 reaches over 82.4 miles and 6 natural lake levels, held by the Colorado Water Conservation Board so that water stays in the stream. Every reach, with its schedule and case →

• East Fork Spring Creek, 8.75 mi: 1.8 (4/1 - 10/31), 1.6 (11/1 - 3/31) cfs (appropriated 2006, 06CW0167) · dossier
• Beaver Creek, 8.7 mi: 1.5 (1/1 - 12/31) cfs (appropriated 1984, 84CW0425) · dossier
• Cow Creek, 7.4 mi: 7.2 (01/01 - 03/31), 20 (04/01 - 04/30), 53 (05/01 - 06/30), 20 (07/01 - 07/31), 15 (08/01 - 08/15), 7.2 (08/16 - 08/28), 5.9 (08/29 - 09/19), 7.2 (09/20 - 12/31) cfs (appropriated 2021, 21CW3064)
• Cow Creek, 7.0 mi: 18 (4/1 - 7/31), 5 (8/1 - 3/31) cfs (appropriated 1984, 84CW0420) · dossier
• West Fork Dallas Creek, 6.3 mi: 2.5 (1/1 - 12/31) cfs (appropriated 1984, 84CW0423) · dossier
• Middle Fork Spring Creek, 6.04 mi: 3.5 (4/1 - 10/31), 1.5 (11/1 - 3/31) cfs (appropriated 2006, 06CW0169) · dossier

and 15 more on the district's instream-flow page.

What the water is like -- USGS sensors right now, where it has been sampled, the impaired-waters list, and how the tap water here stands with EPA -- is on the Water quality tab.

Designated groundwater basins are on their own page.

Source Adjudicated record · verify at DWR water-right transactions ↗ Source Adjudicated record · verify at DWR net amounts ↗

Decreed rights on this network run from 1875-08-01 to 2025-01-27. Of the 20 structures with a yield estimate, the median one’s senior right was in priority 53% of a median irrigation season and 0% in a dry one. 25 abandonment screens and 144 compliance flags are listed below as leads for review — a screen is not an abandonment and a flag is not a violation.

Rights on file: 1583 across 1293 structure(s); 345 structure(s) carry 0 court-case references. Advisory reading aids on public DWR data — not administrative or legal conclusions.

Is the river getting harder to divert from?

Over 2003–2025, administration on this district has been tightening: 1 of 3 measures (days under callA senior water right demanding its water, which requires everyone junior on that stream to stop diverting until it is satisfied., calls set, seniorityColorado shares water by date: the earlier the right, the stronger its claim when the river runs short. "First in time, first in right." of the controlling call) are moving toward more administration, none the other way.

Why diversions stopped — call-based explanations

Sustained diversion stops matched to senior administrative calls.

• CARROLL DITCH (6800519) DWR↗☆ stopped 2025-08-07 (12+ days) — call at MOODY DITCH curtailing 100% of its decreed rate [heuristic-strong]
• DALLAS PLACER DITCH (6800545) DWR↗☆ stopped 2025-08-03 (22+ days) — call at CRAWFORD CLIPPER DITCH curtailing 100% of its decreed rate [heuristic-partial]
• DAINE DITCH (6800542) DWR↗☆ stopped 2025-07-28 (86+ days) — call at MINNESOTA CANAL curtailing 100% of its decreed rate [heuristic-strong]
• BARKER DITCH (6800506) DWR↗☆ stopped 2025-07-22 (99+ days) — call at MINNESOTA CANAL curtailing 90% of its decreed rate [heuristic-partial]
• DOC WADE DITCH (6800559) DWR↗☆ stopped 2025-07-22 (77+ days) — call at MINNESOTA CANAL curtailing 55% of its decreed rate [heuristic-partial]
• CASSIDY DITCH (6800520) DWR↗☆ stopped 2025-07-07 (81+ days) — call at GROVE DITCH curtailing 67% of its decreed rate [heuristic-partial]
• CHAFFEE DITCH (6800523) DWR↗☆ stopped 2025-07-06 (21+ days) — call at GROVE DITCH curtailing 66% of its decreed rate [heuristic-partial]
• BROOKE DITCH (6800510) DWR↗☆ stopped 2025-06-12 (106+ days) — call at MIDKIFF & ARNOLD D curtailing 100% of its decreed rate [heuristic-strong]
• BROWN DITCH (6800511) DWR↗☆ stopped 2025-06-12 (131+ days) — call at MIDKIFF & ARNOLD D curtailing 62% of its decreed rate [heuristic-partial]
• BURGER DITCH (6800513) DWR↗☆ stopped 2025-06-10 (141+ days) — call at MIDKIFF & ARNOLD D curtailing 100% of its decreed rate [heuristic-strong]
• CLIMAX DITCH (6800531) DWR↗☆ stopped 2025-05-22 (21+ days) — call at COAL CREEK DITCH curtailing 100% of its decreed rate [heuristic-strong]
• CANNON DITCH (6800516) DWR↗☆ stopped 2025-05-20 (160+ days) — call at COAL CREEK DITCH curtailing 100% of its decreed rate [heuristic-strong]

Right yield — how often could these rights actually divert?

Share of irrigation-season days each structure's rights were not called out, derived from the 22-year district-scoped call record (senior right = floor, junior right = ceiling constraint). Call-record-derived; DWR's own analysis governs where available.

Abandonment radar (25 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 ~1970 — idleness that begins before then may be unreported use, not nonuse (flagged † below).

• FISHER DITCH (6800577) DWR↗☆ (1904-07-01, 1.2 cfs decreed): last active 1950 — 75 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1970) -- early absence of record is weak evidence of nonuse
• MILLS LATERAL DITCH (6800665) DWR↗☆ (1909-05-01, 0.8 cfs decreed): last active 1950 — 75 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1970) -- early absence of record is weak evidence of nonuse
• WEST SIDE DITCH (6800776) DWR↗☆ (1883-05-01, 2.0 cfs decreed): last active 1950 — 75 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1970) -- early absence of record is weak evidence of nonuse
• ZENA NO 1 SPRING (6800783) DWR↗☆ (1914-01-19, 0.1 cfs decreed): last active 1950 — 75 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1970) -- early absence of record is weak evidence of nonuse
• CATTLE D & WTR SUPPLY (6800521) DWR↗☆ (1967-07-18, 0.5 cfs decreed): last active 1968 — 57 years idle † predates modern reporting era — last recorded activity predates this basin's modern reporting era (~1970) -- early absence of record is weak evidence of nonuse
• KRAFFT DITCH (6800632) DWR↗☆ (1913-11-18, 1.5 cfs decreed): last active 1970 — 55 years idle
• WEBER SPRING POND (6800957) DWR↗☆ (1910-05-01, 0.0 cfs decreed): last active 1971 — 54 years idle
• BEAR GULCH DITCH (6800507) DWR↗☆ (1908-06-01, 5.0 cfs decreed): last active 1974 — 51 years idle
• HUGHES LAKE DITCH (6800611) DWR↗☆ (1911-07-08, 0.5 cfs decreed): last active 1974 — 51 years idle
• PHILLIPS D & WTR SUPPLY (6800689) DWR↗☆ (1963-06-10, 0.6 cfs decreed): last active 1974 — 51 years idle

Compliance screens (144 advisory flags)

Screened 211 of 1293 structures with rights (218 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.

• RIDGWAY RESERVOIR TRI CT (6803675) DWR↗☆: Observed p99 daily rate 504.0 cfs (max 1400.0) exceeds total decreed absolute 133.0 cfs across 75127 recorded day(s).
• ALKALI DITCH D NO 80 (6800501) DWR↗☆: Observed p99 daily rate 45.0 cfs (max 48.0) exceeds total decreed absolute 39.5 cfs across 26106 recorded day(s).
• CHARLEY LOGAN DITCH (6800526) DWR↗☆: Observed p99 daily rate 30.0 cfs (max 39.0) exceeds total decreed absolute 15.7 cfs across 28014 recorded day(s).
• PINION DITCH (6800692) DWR↗☆: Observed p99 daily rate 24.1 cfs (max 29.0) exceeds total decreed absolute 22.7 cfs across 21812 recorded day(s).
• DOC WADE DITCH (6800559) DWR↗☆: Observed p99 daily rate 23.7 cfs (max 27.2) exceeds total decreed absolute 20.5 cfs across 10511 recorded day(s).
• HOMESTRETCH DITCH (6800607) DWR↗☆: Observed p99 daily rate 22.1 cfs (max 26.9) exceeds total decreed absolute 14.0 cfs across 23009 recorded day(s).
• PARK DITCH (6800685) DWR↗☆: Observed p99 daily rate 22.1 cfs (max 25.0) exceeds total decreed absolute 21.0 cfs across 18077 recorded day(s).
• BURKHART EDDY DITCH (6800514) DWR↗☆: Observed p99 daily rate 21.7 cfs (max 28.9) exceeds total decreed absolute 15.0 cfs across 19333 recorded day(s).
• MOODY DITCH (6800668) DWR↗☆: Observed p99 daily rate 21.3 cfs (max 37.2) exceeds total decreed absolute 9.9 cfs across 28465 recorded day(s).
• HOSNER BROWNYARD DITCH (6800609) DWR↗☆: Observed p99 daily rate 20.0 cfs (max 25.0) exceeds total decreed absolute 13.1 cfs across 23694 recorded day(s).

Seniority (top structures by decreed rate)

Recent inventory & legal-document changes

• 2026-09-04 — call set: GALLOWAY DITCH (39410)
• 2026-09-04 — call released: 39314
• 2026-09-03 — call set: PAONIA DITCH (39405)
• 2026-09-03 — call set: CRAWFORD CLIPPER DITCH (39401)
• 2026-09-03 — call released: 39364
• 2026-09-03 — call released: 39310

Water-court filings this month (division-wide)

15 applications in the 2026-08 resume for this basin's division — new rights, changes, augmentation plans — from the water clerk's statutory monthly notice (C.R.S. 37-92-302), the earliest public signal of a new claim. Filings are division-wide, not district-filtered: check the county column. Full resume PDF at the Judicial Branch →

Anyone affected may file a statement of opposition until 2026-10-31 (48 days left). C.R.S. 37-92-302(3): due by the last day of the second month following the filing month — computed, not legal advice; confirm with the water clerk.

Active substitute water supply plans in this district

Temporary State Engineer approvals to divert out of priority (37-92-308 / 37-90-137). A structure operating under one behaves differently under a call than its decreed rights alone suggest — the priority tables above don't know about these; this list does. Source: DWR’s active-SWSP register, refreshed nightly.

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.

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.