Water Intelligence Brief · Archive
August 10, 2026
August 10, 2026 | Sevier River Basin
Snowpack across Sanpete County's contributing watersheds has fully melted out, with all monitored SNOTEL stations reading 0.0" SWE — a normal seasonal condition for early August, though the 2026 season was defined by meltout occurring 4–6 weeks ahead of the historical median meltout date. Streamflow on the Sevier River shows a mixed picture across the basin, with in-county Manti Creek running at minimal levels and divergent conditions at upstream and downstream gauges. Reservoir storage data and 7-day forecast details are available in the full brief.
All six SNOTEL stations monitored in Sanpete County's contributing watersheds are reporting 0.0" snow water equivalent (SWE) as of August 9, 2026, which is the expected seasonal condition for this point in the calendar — the historical median SWE for these stations in early August is also 0.0". No percent-of-median figures are reported for any station, confirming that current readings reflect normal end-of-season conditions rather than a deficit relative to typical August levels.
Station-by-station readings:
The critical context for 2026 is not today's SWE reading — it is timing. These stations melted out 4–6 weeks ahead of the historical median meltout date, driven by an anomalous March heat wave across the Mountain West. That early meltout has shaped the entire irrigation season: spring runoff peaked and receded earlier than normal, reducing the window for reservoir filling and early-season carryover. With snowpack now fully absent and no new accumulation expected until fall, streamflow and stored water are the only remaining supply variables for the balance of the irrigation season.
Manti Creek below Dugway Creek, near Manti (the only active USGS streamflow gauge within Sanpete County), was recorded at 3 cfs and falling as of August 7. This represents minimal late-season flow and is the primary in-county streamflow indicator for local irrigators. No active gauge exists on the San Pitch River mainstem — users relying on San Pitch drainage should contact Sanpete Water Conservancy District for any supplemental local monitoring data.
Sevier River basin gauges in adjacent counties provide broader context for system-wide conditions:
The contrast between the Kingston reading (2 cfs, falling) and the Lynndyl reading (196 cfs, stable) underscores the complexity of the Sevier River system, where diversions, return flows, and reservoir operations can produce conditions that vary dramatically along the river's length. Sanpete County users are most directly affected by the Manti Creek and Kingston-area reach conditions, both of which reflect the tight late-season supply environment typical of an early-meltout year.
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Data Sources: SNOTEL data through August 9, 2026; USGS streamflow data through August 10, 2026
Data Current As Of: Utah Division of Water Rights
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, and Utah Division of Water Resources 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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