Water Intelligence Brief · Archive
July 6, 2026
Eastern Juab Valley Agricultural Corridor — July 6, 2026
Salt Creek is flowing at 6–7 cfs and falling, reflecting the tail end of Mount Nebo snowmelt runoff in what was an extremely early-melt year across the Mountain West. Snowpack that historically feeds local streams into July melted out 4–6 weeks ahead of the historical median meltout date, meaning the primary seasonal recharge pulse for Salt Creek and Currant Creek is effectively complete. Reservoir storage data and 7-day forecast details are available in the full brief.
Juab County has no active SNOTEL station on or near Mount Nebo. This is a meaningful monitoring gap — Mount Nebo (11,928 ft), the highest peak in the Wasatch Range, sits directly above the eastern Juab Valley and provides the primary snowmelt that feeds both Salt Creek and Currant Creek. Without an in-county station, local irrigators cannot directly track remaining snowpack from SNOTEL data alone.
No SNOTEL readings are available for Juab County in today's data. For the closest proxy monitoring, the Payson Ranger Station SNOTEL in Utah County (to the north) provides the most relevant neighboring reference. At this point in the season — July 6 — any remaining snowpack in the Mount Nebo area would be minimal under normal conditions. Given 2026's anomalous early-melt pattern, driven by a March heat wave, snowpack in this elevation band melted out 4–6 weeks ahead of the historical median meltout date. The seasonal snowmelt contribution to Salt Creek is effectively exhausted.
Contact the Utah Division of Water Resources for seasonal snowpack assessments specific to the Salt Creek watershed.
Salt Creek at Nephi (primary local indicator): 6 cfs, falling. This gauge directly reflects Mount Nebo melt and Salt Creek watershed runoff available to Nephi-area irrigators. The falling trend confirms that the snowmelt pulse has passed and flows are declining into base-flow conditions typical of mid-to-late summer.
Salt Creek Below Nephi Powerplant Diversion: 7 cfs, stable. The slight difference between this reading and the upstream gauge reflects the powerplant diversion structure — this is the post-diversion flow reaching downstream users.
Currant Creek near Mona: 1 cfs, falling. Currant Creek is effectively at minimum flow for the season. Users dependent on this source should plan accordingly.
Regional context — Sevier River near Juab: 258 cfs, stable. This gauge reflects conditions across the entire upstream Sevier River basin (over 5,000 square miles), including contributions well outside Juab County. It is not a local supply indicator — use it for broad basin context only.
Sevier River near Lynndyl: 263 cfs, falling. Consistent with the Juab gauge, confirming stable-to-slightly-declining regional flows through the lower basin.
Other gauges in today's data — Manti Creek, Sevier River at Hatch, Kingston, and Sigurd — are outside the eastern Juab Valley corridor and are provided for regional basin reference only.
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Data Sources: SNOTEL data through July 5, 2026; USGS streamflow data through July 6, 2026
Data Current As Of: July 6, 2026
Important Disclaimers: This brief provides automated analysis for informational purposes only. Specific numerical claims have not been independently verified. Consult official sources including your local water district, Utah Division of Water Rights (primary regulator for all Juab County water rights), Utah Division of Water Resources (for Yuba Lake / Sevier Bridge Reservoir storage data), and local irrigation companies including Nephi Irrigation Company, for regulatory decisions and water rights administration.
Data & Disclaimers
Sources: NRCS SNOTEL network · USGS National Water Information System · National Weather Service
This brief provides automated analysis for informational purposes only. Consult official sources including your local water district and state Division of Water Rights for regulatory decisions. This document does not constitute legal, regulatory, or engineering advice.
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