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North Fork/Tribs.

Division 4 · Water District 40
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North Fork/Tribs. on the ground — the ditches, wells, reservoirs and gages of Water District 40 · clicktap anything for its record

Snowpack — no snow on the ground at 3 SNOTEL sites — normal for the date; the snow year begins in October and typically peaks around April 4. Runoff outlook — Paonia Reservoir Inflow: even odds of at least 2 kAF over 06-01 to 06-30 — 15% of a normal season, per NRCS, issued 2026-06-01 — the season’s final; new forecasts begin in January. Runoff outlook — NF Gunnison R nr Somerset: even odds of at least 21 kAF over 06-01 to 07-31 — 23% of a normal season, per NRCS, issued 2026-06-01 — the season’s final; new forecasts begin in January. Runoff outlook — Surface Ck at Cedaredge: even odds of at least 1 kAF over 06-01 to 07-31 — 26% of a normal season, per NRCS, issued 2026-06-01 — the season’s final; new forecasts begin in January. Full snow & runoff picture — charts, forecast history and how the forecasts have verified →

Sites, exceedance bands and sources
SNOTEL siteElev (ft)SWE (in)Median (in)% of medianTypical peak
Mc Clure Pass8760 0.00.0 April 4 (16.6 in)
Overland Res.9890 0.10.0 April 5 (12.4 in)
Park Reservoir9990 0.00.0 April 26 (27.4 in)

Paonia Reservoir Inflow — 06-01 to 06-30 volume, thousand acre-feet (chance the volume is AT LEAST this):

90%70%50%30%10%Normal
01247 13

NF Gunnison R nr Somerset — 06-01 to 07-31 volume, thousand acre-feet (chance the volume is AT LEAST this):

90%70%50%30%10%Normal
1217213862 91

Surface Ck at Cedaredge — 06-01 to 07-31 volume, thousand acre-feet (chance the volume is AT LEAST this):

90%70%50%30%10%Normal
11124 5

Snow-water equivalent and medians (1991–2020) from NRCS SNOTEL; seasonal volume forecasts from the NRCS National Water and Climate Center. Sites and forecast points are assigned to the district whose boundary contains them — snowpack that feeds this district can also sit in a neighboring headwater district. Toggle the Snow chip on the map above to see the sites.

Topology cross-check: 14 parent disagreements, 3 sizable streams not on this network (vs DWR's route framework — under review)

This flow network was built mechanically; DWR's Source Water Route Framework disagrees with it in the places below. Each row is a question a human reviewer has not yet answered — not an error verdict. Checked 29 streams, 15 agree. Know this water? Tell us →

StreamThis site routes it toDWR routes it to
Kiser Creek the mainstem Ward Creek
Ward Creek the mainstem Tongue Creek
Youngs Creek the mainstem Kiser Creek
Currant Creek the mainstem Gunnison River
Hubbard Creek the mainstem North Fork Gunnison River
Dirty George Creek the mainstem Tongue Creek
Happy Hollow Creek the mainstem Tongue Creek
Leroux Creek the mainstem North Fork Gunnison River

Sizable streams DWR maps here that this network does not carry:

Milk Creek (8 mi) · Marcott Creek (6 mi) · Caesar Creek (3 mi)

Full diagnostic snapshot pending — this district's weekly-style report (system status, active calls, hydrographs, anomaly flags) is produced by the nightly rotation and appears here after its first run. The tabs above are live now.

Groundwater

1,355 water-level measurements across 99 monitored well(s) — 47 alluvial, 10 bedrock — plus 3 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.

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

Fastest-declining wellsSettingft / decadeSpanp
WS-47 bedrock -8.07 30 yr 0.0021
WS-27 bedrock -1.82 31 yr 0.0077

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.