Lower Uncompahgre River

Evolution of the network

Gage flow trend & changepoints

What counts as a trend here

Computed 2026-08-20 08:57 from 30 gage(s) with cached period-of-record data. Mann-Kendall (trend) and Pettitt (changepoint) both require at least 8 years spanning at least 10 years of record. A gage below that reports no signal — which is not the same as “no change.”

Of the 30 gages with enough record, 4 are trending down and 2 up, and 4 carry a detected shift. The clearest is ABC LATERAL, -39.6 points of its long-term median per decade over 40 years (p<0.0001). The other 24 show no clear signal either way.

Gage	Trend	Change / decade points of median	Significance	Years	Changepoint
▸ SELIG CANAL☆ SELGCNCO	↓ decreasing	-148.0	p=0.018	15	~2019
▸ UNCOMPAHGRE RIVER UPSTREAM OF SOUTH CANAL☆ UNCUPSCO	↓ decreasing	-48.3	p=0.036	17	~2017
▸ ABC LATERAL☆ ABCLATCO	↓ decreasing	-39.6	p=0.000	40	~2013
▸ SOUTH CANAL NEAR MONTROSE☆ SOUCANCO	↑ increasing	+23.5	p=0.002	36	—
▸ MONTROSE & DELTA CANAL☆ MANDCNCO	↓ decreasing	-13.8	p=0.003	15	—
▸ UNCOMPAHGRE RIVER AT DELTA, CO.☆ UNCDELCO	↑ increasing	+2.8	p=0.048	88	~1981

24 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. 28 gage(s) and 61 structure(s) report in 2026, but structure reporting only reached half its modern level around ~1950. 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)
1900s	0	1
1930s	1	2
1940s	1	0
1950s	1	57
1960s	1	70
1970s	1	74
1980s	1	72
1990s	4	68
2000s	5	52
2010s	15	63
2020s	23	61

Mass-balance (network closure) trend

Structure divrec-history backfill coverage as of the last check: 7% of 460 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 (1991–2026)

Mass-balance kinks computed for every summer month back to 1991 (854 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.

• FAIRVIEW INLET OFF THE SOUTH CANAL NEAR MONTROSE: reach shifted from -350 cfs to -95 cfs summer mean (more gaining, p=0.000, 17 yr) [alluvial valley: real alluvial aquifer -- a decades-long shift toward losing is the classic signature of alluvial pumping and urbanization] [1 alluvial wells within 2 mi of the gage; pooled water table -0.5 ft (2014–2024, decreasing)]
• UNCOMPAHGRE RIVER NEAR OLATHE: reach shifted from +108 cfs to -187 cfs summer mean (more losing, p=0.002, 25 yr) [alluvial valley: real alluvial aquifer -- a decades-long shift toward losing is the classic signature of alluvial pumping and urbanization]
• GARNET DITCH: reach shifted from -63 cfs to -18 cfs summer mean (more gaining, p=0.000, 16 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=-0.69) -- part of it may be unaccounted water becoming accounted, not hydrologic change] [3 alluvial wells within 2 mi of the gage; pooled water table -0.3 ft (2014–2024, no_trend)]
• IRONSTONE CANAL NEAR OLATHE, CO: reach shifted from +124 cfs to +164 cfs summer mean (more gaining, p=0.010, 16 yr) [alluvial valley: real alluvial aquifer -- a decades-long shift toward losing is the classic signature of alluvial pumping and urbanization] [3 alluvial wells within 2 mi of the gage; pooled water table +1.2 ft (1976–2024, no_trend)]

Groundwater now has its own tab: 76 monitored well(s), water-table trends, stream corridors, and the advisory depletion screen.

Reservoirs now has its own tab: 3 reservoir(s), end-of-year storage back to 1950, click-to-chart histories.

Cross-gage pattern fingerprint

Over the 35-year window with full coverage (1992–2026), the dominant shared pattern across 3 gage(s) explains 63% of year-to-year variance (almost certainly a basin-wide climate/snowpack driver).

ABCLATCO doesn't move with that shared pattern -- a real, localized signal (a new diversion, land-use change, or a gage-specific data problem) worth a closer look, not necessarily noise.

8,080 water-level measurements across 76 monitored well(s) — 64 alluvial, 0 bedrock — plus 0 administered well(s) reporting metered pumping.

What is being counted

Observation wells and pumping wells are different populations and are never conflated: water levels come from monitored observation wells, and metered pumping comes from administered wells reporting through diversion records. Click any well to chart its own record.

Well map

3D aquifer x-ray

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

Load 3D x-ray

How the surfaces are built, and what they are not

Alluvial water table on top, Denver Basin members (Dawson, Denver, Arapahoe, Laramie–Fox Hills) stacked beneath where measured, interpolated from measured water levels. Units are never mixed; a surface exists only inside its own unit's well coverage, with no extrapolation; thin epochs are suppressed and say why. Vertical scale is exaggerated for readability and z is head elevation in feet. These are measured heads, not a calibrated groundwater model.

Water-table trends

Of 28 well(s) with enough record for a trend test: 6 declining, 2 rising.

Fastest-declining wells	Setting	ft / decade	Span	p
▸ LGRB-Poly 30☆	alluvial	-2.87	10 yr	0.0491
▸ NC04900936BA LGRB Poly 28☆	alluvial	-2.79	11 yr	0.0051
▸ LGRB-Poly 23☆	alluvial	-2.74	10 yr	0.0042
▸ NC05101035BD LGRB Poly 8☆	alluvial	-2.64	12 yr	0.0236
▸ LGRB-Poly 19☆	alluvial	-2.1	10 yr	0.02
▸ LGRB-Poly 6☆	alluvial	-1.44	10 yr	0.0491

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.

How the corridor is assembled

For each reach whose gain/loss has shifted (Trends tab): the wells within 2 miles of its anchoring gage, their pooled water-table history over the same era, and an advisory Glover screen of lagged stream depletion from nearby metered pumping. v1 proximity = distance to the reach's anchoring gage; segment-based reach join is a flagged upgrade.

FAIRVIEW INLET OFF THE SOUTH CANAL NEAR MONTROSE: 1 alluvial well(s) nearby; pooled water table -0.5 ft (2014–2024, decreasing, p=0.0491)

UNCOMPAHGRE RIVER NEAR OLATHE: 3 alluvial well(s) nearby

GARNET DITCH: 3 alluvial well(s) nearby; pooled water table -0.3 ft (2014–2024, no_trend, p=0.5915)

IRONSTONE CANAL NEAR OLATHE, CO: 3 alluvial well(s) nearby; pooled water table +1.2 ft (1976–2024, no_trend, p=0.0584)

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.

3 reservoir(s) with 58 storage measurement(s), 1950–2022.

Why storage matters to the flow network

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?

What “full” is measured against

Bubble size is proportional to a reservoir's record-high storage. Fill is its 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 as a share of its own record high otherwise. A wrong capacity would be worse than an honest record high, so only confident joins upgrade.

A dashed teal ring marks reservoirs reporting live DWR telemetry: their fill reflects yesterday's storage, is drawn as a dotted tail on charts, and is treated as provisional until the next verified HydroBase snapshot supersedes it.

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
▸ CITIZENS RESERVOIR (4103651) ☆	123	1956-09-01
▸ MOCK RESERVOIR NO 1 (4103653) ☆	40	1952-05-01
▸ BUCKHORN RESERVOIR #2 (4103650) ☆	0	2022-09-02

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.

Or enter an administration number directly

Administration number
Simulate

DWR administration numbers encode appropriation and adjudication dates; lower is more senior.