Water Intelligence Brief · Archive

Gooding County, ID

September 7, 2026

Gooding County Water Intelligence Brief

September 7, 2026 | Free-Tier Edition


Situation Summary

Snake River canal deliveries and ESPA spring discharge are both in late-season operational mode, with the Malad River near Gooding holding at 148 cfs — a stable reading that supports continued trout aquaculture operations in the Hagerman Valley as of this week. Dairy operators and alfalfa producers relying on Snake River irrigation should monitor delivery scheduling closely as the season winds toward shutdown, given that snowpack-driven tributary inflows from the Big Wood system are now exhausted for the year. Reservoir storage data and 7-day forecast details are available in the full brief.


Snowpack Conditions

Both SNOTEL stations reporting for Gooding County's primary tributary watershed show complete meltout, which is normal and expected for early September.

  • Galena Summit (490:ID:SNTL), September 6: Snow water equivalent 0.0", snow depth 2.0". The residual depth reading likely reflects instrument artifact — no meaningful snowpack remains. This station monitors Big Wood River headwaters and is the primary local tributary indicator for Gooding County. The 2026 snowpack at Galena Summit melted out 4–6 weeks ahead of the historical median meltout date, meaning tributary inflow pulses to the Snake River from the Big Wood system peaked and concluded well ahead of the normal seasonal window.
  • Lewis Lake Divide (September 6): SWE 0.0", depth 0.0". Full meltout, no snowpack remaining.
  • At this point in the calendar, 0.0" SWE reflects normal seasonal conditions — the median SWE for both stations on this date is also 0.0". The operational story is not current snowpack deficit; it is the legacy of early-season meltout that moved tributary contributions into the system weeks ahead of schedule and reduced late-summer inflow buffering.


    Streamflow Conditions

    Malad River near Gooding (USGS 13152500), September 7: 148 cfs, stable.

    This is the defining gauge for Gooding County's water supply picture. The Malad River near Gooding is the primary indicator of ESPA spring discharge for the Hagerman Valley — its flow reflects the Thousand Springs complex, where Eastern Snake Plain Aquifer groundwater emerges from the Snake River canyon walls and discharges directly into the system. Unlike snowmelt-driven tributaries, this flow is relatively stable year-round, governed by aquifer level and spring discharge rate rather than seasonal precipitation or snowpack.

    The current 148 cfs stable reading indicates steady ESPA spring discharge, supporting normal operational conditions for Hagerman Valley trout aquaculture this week. Trout farm operators holding IDWR spring water appropriations should note that any meaningful change in this gauge — rather than snowpack data or canal delivery schedules — is their primary supply signal.

    For dairy operators and alfalfa producers on Snake River canal deliveries, the relevant mainstem context comes from upstream gauges at Milner and Twin Falls. The Big Wood River tributary contribution, governed by Galena Summit snowpack, is now seasonally exhausted.


    Seasonal Guidance

  • Contact Idaho Department of Water Resources (IDWR), Eastern Regional Office to verify current spring water appropriation status and ESPA monitoring updates relevant to Hagerman Valley trout operations and dairy spring water permits.
  • Reach out to your local canal company or water district serving Gooding County acreage to confirm late-season delivery schedules and any anticipated curtailment or shutoff timing.
  • Check with USBR Pacific Northwest Region, Boise office for upstream Snake River storage and operational context that governs late-season mainstem flows into the Gooding area.
  • Monitor the USGS Malad River near Gooding gauge (13152500) directly at waterdata.usgs.gov for any change in spring discharge rate — the key early signal for Hagerman Valley trout aquaculture operators.

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


    Data Sources: SNOTEL data through September 6, 2026; USGS streamflow data through September 7, 2026

    Data Current As Of: September 7, 2026. SNOTEL data sourced from NRCS National Water and Climate Center. Streamflow data sourced from USGS National Water Information System.

    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; Idaho Department of Water Resources (IDWR — administers Water District 36 for middle Snake River and tributary water rights, and administers separate spring water appropriations for Hagerman Valley trout aquaculture and dairy operations); Idaho Department of Fish and Game (co-manages Thousand Springs State Park area); and U.S. Bureau of Reclamation, Pacific Northwest Region, Boise office, for upstream storage and operational context. For water rights administration and regulatory decisions, contact IDWR directly.

    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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