Water Intelligence Brief · Archive
August 17, 2026
August 17, 2026 | Free-Tier Edition
Caribou County enters the late-irrigation season with snowpack fully melted across all monitored SNOTEL stations — a condition that arrived 4–6 weeks ahead of the historical median meltout date following the anomalous March heat wave. Bear River mainstem flows remain active through the system, though several tributary gauges show falling or modest readings consistent with late-season conditions. Reservoir storage data, 7-day forecast details, and depletion analysis are available in the full brief.
All eight SNOTEL stations serving Caribou County watersheds are reporting effectively zero snow water equivalent as of August 16, 2026 — a normal condition for this calendar date, as the historical median SWE at these stations is also 0.0" by mid-August. The notable story for 2026 is not today's readings, but timing: these stations melted out 4–6 weeks ahead of their historical median meltout dates, meaning the snowpack-driven recharge pulse entered streams and soils significantly earlier in the season than typical.
Station-by-station readings:
The trace readings at Emigrant Summit (0.2" SWE) and Giveout (0.3" SWE), combined with a residual depth reading at Franklin Basin (1.0"), are minor anomalies and do not represent meaningful snowmelt contribution at this stage of the season. No meaningful snowpack-driven streamflow augmentation should be anticipated from the monitored network going forward. Late-season streamflow will reflect reservoir releases, baseflow, and any precipitation events rather than snowmelt input.
Ten USGS gauges across Caribou County's four watersheds provide the current streamflow picture. The Bear River mainstem shows the most substantial flows, while tributary and secondary basin gauges reflect typical late-season low-flow conditions.
Bear River Basin:
Blackfoot River Basin:
Portneuf River Basin:
Salt River Basin:
The Malad River gauge data (last reading 05/15) is stale and should not be used for current operational decisions. Users dependent on Malad River conditions should contact USGS or IDWR directly for current status. The divergence between falling flows at Pescadero and rising flows at Corinne on the Bear River mainstem may reflect system storage releases or tributary inputs between gauges — water managers with diversion rights in that reach should monitor closely.
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Data Sources: SNOTEL data through August 16, 2026; USGS streamflow data through August 17, 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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