Water Intelligence Brief · Archive

Washington County, UT

June 22, 2026

Washington County Water Intelligence Brief

June 22, 2026 | Virgin River Basin | Free-Tier Edition


1. Situation Summary

Washington County's municipal water supply enters peak summer demand season with snowpack fully melted across all Virgin River basin headwater stations — a condition that arrived 4–6 weeks ahead of the historical median meltout date following an anomalous March heat wave. Streamflows across the Virgin River system are declining or stable at low-to-moderate levels, consistent with a post-peak-runoff summer baseline, with the primary surface water buffer now shifting to WCWCD-managed in-county reservoir storage at Quail Creek and Sand Hollow. Reservoir storage data, 7-day forecast details, and depletion trajectory analysis are available in the full brief.


2. Snowpack Conditions

All five SNOTEL stations monitoring the Virgin River basin headwaters report fully melted conditions as of June 21, 2026. This is expected for this calendar date — median SWE for late June at these elevations is also 0.0" — but the significance lies in timing: meltout occurred 4–6 weeks ahead of the historical median meltout date, meaning the snowpack's contribution to spring runoff concluded substantially earlier than normal this year.

| Station | SWE (in) | Snow Depth (in) |

|---|---|---|

| Gardner Peak | 0.0 | 0.0 |

| Gutz Peak | 0.0 | 0.0 |

| Kolob | 0.0 | 0.0 |

| Long Valley Jct | 0.0 | 3.0 |

| Webster Flat | 0.0 | N/A |

One anomaly warrants noting: Long Valley Junction reports 3.0 inches of snow depth despite 0.0" SWE, which may reflect a sensor artifact or residual compacted granular material — this reading does not represent meaningful water-equivalent storage. Washington County's SNOTEL network is sparser than northern Utah counties, and monitoring coverage of the higher-elevation Virgin River basin headwaters is limited; users should treat these five stations as directional indicators rather than a comprehensive snowpack census.

The practical consequence for municipal managers: the snowmelt pulse that typically supplements late-spring reservoir inflows has already concluded. No additional snowmelt contribution to streamflow or reservoir storage should be expected for the remainder of the summer season. WCWCD reservoir storage and monsoon precipitation timing are now the operative supply variables.


3. Streamflow Conditions

Six USGS gauges across the Virgin River basin provide current streamflow context as of June 22, 2026.

Virgin River mainstem and major forks:

  • East Fork Virgin River near Springdale: 39 cfs — stable. Represents post-runoff baseflow conditions on one of the system's primary upper tributaries.
  • North Fork Virgin River near Springdale: 29 cfs — falling. Declining trend consistent with early-melt year and advancing summer baseflow recession.
  • Virgin River at Virgin: 58 cfs — stable. The integrated upper mainstem signal; relatively steady but reflecting consolidated low-to-moderate summer conditions.
  • Virgin River above La Verkin Creek near La Verkin: 33 cfs — falling. The falling trend here, downstream of the Virgin gauge, warrants attention — the step-down in volume between Virgin (58 cfs) and La Verkin (33 cfs) likely reflects intervening diversions and channel losses.
  • Santa Clara River system:

  • Santa Clara River near Pine Valley: 6 cfs — falling. Upper Santa Clara flows are declining, consistent with post-melt recession.
  • Santa Clara River at St. George: 2 cfs — stable. Near-baseflow conditions at the downstream St. George gauge; essentially the lowest functional flow level for this reach. Municipal and agricultural planners relying on Santa Clara surface water should treat this as a low-supply baseline for the coming months.
  • System-wide interpretation: Across all six gauges, the pattern is consistent with an early-melt year in late-season baseflow mode. No gauges show elevated or rising flows. The falling trend at the North Fork, La Verkin, and Pine Valley stations confirms the basin is past peak runoff and receding into summer minimum conditions earlier in the calendar year than typical. For a rapidly growing metro area, this accelerates the timeline at which reservoir storage becomes the primary operational buffer — a condition WCWCD managers should factor into drawdown planning for July through September.


    4. Seasonal Guidance

  • Contact Washington County Water Conservancy District (WCWCD) directly at wcwcd.org to verify current operational status of Quail Creek and Sand Hollow reservoirs and any active conservation measures in effect for summer 2026.
  • Check Utah Division of Water Rights (waterrights.utah.gov) for current administrative status of Virgin River surface water rights, Navajo Sandstone groundwater permits, and any filings relevant to Shivwits Band of Paiutes water rights administration in Washington County.
  • Agricultural users in Hurricane Valley and the Enterprise area should contact the Virgin River Valley Water Users Association or local ditch company representatives for current delivery scheduling and any pro-rata adjustments in effect given declining Santa Clara and Virgin River flows.
  • Monitor Colorado River Basin updates through the Bureau of Reclamation Lower Colorado Region (usbr.gov/lc) for ongoing Lower Basin shortage tier status, Lake Powell operational conditions, and Lake Powell Pipeline federal review developments relevant to Washington County's long-term supply planning.

  • Subscribe for the full brief including reservoir storage, weather forecasts, depletion analysis, and detailed operational recommendations.


    Data Sources: SNOTEL data through June 21, 2026; USGS streamflow data through June 22, 2026.

    Data Current As Of: June 22, 2026. Utah Division of Water Rights administrative records reflect most recent published updates.

    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), Utah Division of Water Rights, and Bureau of Reclamation Lower Colorado Region for regulatory decisions and water rights administration. Colorado River Compact obligations and Lower Basin shortage conditions are subject to federal administrative determinations outside the scope of this brief. This document 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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    Washington County UT Water Report — June 22, 2026 | Wai AI