Water Intelligence Brief · Archive
July 20, 2026
July 20, 2026 | Virgin River Basin | Free-Tier Edition
Washington County's municipal water supply enters the heart of summer demand season drawing on WCWCD-managed surface storage and Navajo Sandstone groundwater, with snowpack contributing no active melt at this date — consistent with seasonal expectations, though the 2026 water year was defined by an anomalous early meltout 4–6 weeks ahead of the historical median. Virgin River mainstem and tributary flows show a mixed picture of rising and stable conditions typical of mid-July monsoon onset dynamics. Reservoir storage data, 7-day forecast details, and depletion trend analysis are available in the full brief.
All five SNOTEL stations monitoring the Virgin River basin headwaters are reporting zero snow water equivalent and zero snow depth as of July 19, 2026 — which accurately reflects normal mid-July conditions for southwest Utah. This is not a below-normal signal for this calendar date; the median SWE at each of these stations is also 0.0" in mid-July, so no deficit language applies to current readings.
The meaningful snowpack story for 2026 is timing, not current depth. All five stations — Gardner Peak, Gutz Peak, Kolob, Long Valley Junction, and Webster Flat — melted out 4–6 weeks ahead of their historical median meltout dates, driven by an anomalous March heat wave that accelerated snowmelt across the Mountain West. That early meltout compressed the spring runoff pulse, likely reducing total recharge to both surface storage and the Navajo Sandstone aquifer compared to a normal melt-season pattern.
It is worth noting that southwest Utah has sparser SNOTEL coverage than northern Utah counties, and the five stations listed represent the practical limit of high-elevation snowpack monitoring in the Virgin River basin headwaters. This monitoring gap is a standing data limitation for WCWCD's supply planning.
Six USGS gauges provide current flow intelligence across the Virgin River basin:
The rising trend on the East Fork, North Fork, La Verkin reach, and Pine Valley gauge is consistent with early monsoon precipitation or localized convective runoff typical of mid-July in southwest Utah. The Virgin River at Virgin is falling at 75 cfs, suggesting the mainstem above the tributary confluences has not yet responded to the same pulse affecting downstream and tributary gauges — or that an earlier pulse is receding at that location.
The Santa Clara River at St. George holding at just 2 cfs (stable) is the most operationally significant reading for near-term municipal supply: the Santa Clara system feeds into WCWCD's service area and this low mainstem flow at the St. George gauge underscores continued dependence on stored water in Quail Creek and Sand Hollow reservoirs during peak summer demand. The Pine Valley tributary at 13 cfs rising suggests some upstream contribution that has not yet materialized at the downstream St. George gauge.
Monsoon-season flows in this basin are episodic and can shift significantly within 24–72 hours. Managers should not treat the current rising trend on tributary gauges as a sustained supply signal without monitoring continuity.
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Data Sources: SNOTEL data through July 19, 2026; USGS streamflow data through July 20, 2026
Data Current As Of: July 20, 2026 | 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, Washington County Water Conservancy District (WCWCD, primary water authority for Quail Creek and Sand Hollow reservoirs), the Utah Division of Water Rights, and the Bureau of Reclamation Lower Colorado Region for regulatory decisions and water rights administration. Colorado River Compact obligations and ongoing Lower Basin shortage conditions may affect Washington County's long-term supply posture; the proposed Lake Powell Pipeline remains dormant pending federal review and Colorado River system resolution. The Shivwits Band of Paiutes holds recognized water rights in Washington County — water managers and planners should account for tribal water rights in any supply planning or rights administration context. This brief does not constitute legal, engineering, or water rights advice.
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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