Water Intelligence Brief · Archive
June 22, 2026
June 22, 2026 | Bear River Basin & Tributaries
Caribou County enters late June 2026 with snowpack effectively gone across all monitored SNOTEL stations, reflecting an extremely early meltout season — stations melted out 4–6 weeks ahead of historical median meltout dates following an anomalous March heat wave. Streamflow patterns are mixed, with the Bear River at Pescadero running notably high while upper and lower Bear River gauges show falling conditions, suggesting active system management and storage operations are influencing local delivery conditions. Reservoir storage data, 7-day forecast details, and depletion trajectory analysis are available in the full brief.
All eight SNOTEL stations serving Caribou County's watersheds are reporting at or near zero snow water equivalent as of June 21, 2026 — a condition that reflects the early-melt character of the 2026 season rather than an anomalous single-day reading.
Station Readings:
The near-universal 0.0" SWE readings are consistent with the normal seasonal condition for late June — at this point on the calendar, median SWE is also 0.0" at most stations, meaning the snowpack is not below normal *today* but melted out significantly earlier than the historical median meltout date. Franklin Basin is the sole station carrying any meaningful remaining SWE at 0.6", with 2.0" of snow depth still present. Giveout shows 0.4" SWE with no measurable depth recorded. Tony Grove Lake and USU Doc Daniel report residual snow depth (1.0" and 3.0", respectively) despite 0.0" SWE — indicating very dense or crusted late-season snowpack remnants with minimal free water content remaining.
The practical implication: snowmelt-driven inflow to Bear River basin streams, reservoirs, and the Blackfoot system has largely concluded. Any additional inflow for the remainder of the season will depend on summer precipitation events rather than snowpack release.
Ten USGS gauges across Caribou County's four watersheds provide a complex and varied picture of current conditions.
Bear River Basin:
Blackfoot River Basin:
Portneuf River Basin:
Salt River Basin:
The standout feature is the large disparity between the Bear River at Border (134 cfs, falling) and Bear River at Pescadero (1,550 cfs, rising). Agricultural users dependent on Bear River deliveries through the Pescadero reach should note that this elevated and rising condition may reflect managed releases rather than natural runoff — and conditions can shift with reservoir operational decisions.
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Data Sources: SNOTEL data through June 21, 2026; USGS streamflow data through June 22, 2026
Data Current As Of: Idaho Department of Water Resources (Eastern Regional Office in Pocatello, (208) 525-7161, for Bear River basin counties)
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, U.S. Bureau of Reclamation (for Blackfoot Reservoir), and PacifiCorp/Bear River Commission (for Bear Lake storage) 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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