Bear Lake County, ID — Agricultural Water Intelligence Brief

Issued: April 28, 2026 | Bear River Basin

1. Situation Summary

Bear Lake County faces a significantly stressed water supply outlook entering the 2026 irrigation season. Snowpack across the Bear River Basin is highly variable but predominantly well below seasonal norms, with several monitoring stations already recording zero snow water equivalent — conditions more typical of late spring than late April. The 2026 season has been characterized by an extreme March heat event that drove exceptionally early snowmelt across the Mountain West, stripping moisture reserves that would normally sustain streamflows through the critical summer irrigation period. While a small number of higher-elevation stations retain meaningful snowpack, agricultural water users should plan for reduced late-season surface water availability and heightened water rights administration risk throughout the basin.

2. Snowpack Conditions

Snowpack conditions across the Bear River Basin watershed serving Bear Lake County present a deeply mixed and predominantly concerning picture as of April 27, 2026.

Stations at zero snowpack:

- Bear River RS: 0.0" SWE (0% of 1.4" median)

- Emigrant Summit: 0.0" SWE (0% of 19.2" median) — notably, this station's median at this date is nearly 20 inches, making the complete absence of snow particularly significant

- Giveout: 0.0" SWE, 0.0" depth

- Slug Creek Divide: 0.0" SWE (0% of 7.2" median)

Stations with severely reduced snowpack:

- Garden City Summit: 0.8" SWE (6% of 12.8" median), 5.0" depth — effectively depleted

Stations retaining meaningful snowpack:

- Franklin Basin: 14.1" SWE (57% of 24.6" median), 31.0" depth

- Tony Grove Lake: 16.9" SWE (54% of 31.1" median), 42.0" depth

- USU Doc Daniel: 20.7" SWE (71% of 29.1" median), 59.0" depth — the strongest reading in the basin

The three higher-elevation stations retaining snowpack offer some buffer for near-term runoff, but the majority of monitoring points have already exhausted their snowpack reserves. The overall basin picture is one of significantly below-normal accumulated water storage, with limited remaining snowmelt contribution expected as the season progresses into May and June.

3. Streamflow Conditions

Current streamflow readings from USGS gauges across the Bear River Basin as of April 28, 2026 show a basin that is active but fragmented in its flow picture.

- Bear River at Border, WY: 167 cfs, rising — upstream inflow to the basin is increasing, likely reflecting snowmelt contribution from the higher-elevation stations still holding snow

- Bear River at Pescadero, ID: 94 cfs, stable — flow within the county corridor is modest and holding steady

- Bear River near Corinne, UT: 1,330 cfs, stable — substantially higher flows at the lower basin reflect cumulative contributions from multiple tributaries

- Blacksmith Fork above Upper and Lower Canal Dam near Hyrum, UT: 68 cfs, stable

- Little Bear River at Paradise, UT: 112 cfs, rising

- Logan River above State Dam, near Logan, UT: 237 cfs, stable

- Malad River near Bear River City, UT: 5 cfs — minimal tributary contribution

The rising signal at the Border, WY gauge and on the Little Bear River suggests the remaining high-elevation snowpack is beginning to contribute to runoff. However, given how reduced the overall snowpack reservoir is, this pulse is likely to be shorter in duration than in normal years.

4. Key Reservoir Systems

The primary reservoir systems relevant to Bear Lake County agricultural water supply include:

- Bear Lake — The dominant regional multi-year storage facility for the Bear River system. Bear Lake is managed under a FERC license (P-20) held by PacifiCorp in coordination with the Bear River Commission. It is not a Bureau of Reclamation facility. Current storage status should be verified directly with PacifiCorp or the Bear River Commission.

- Montpelier Reservoir — A smaller local storage facility on Montpelier Creek serving localized agricultural users in the Montpelier area.

Water users are encouraged to contact PacifiCorp's Bear River operations and the Bear River Commission directly for current storage levels, as capacity figures are not available in this brief. Do not rely on informal estimates for operational planning.

5. Water Rights Administration Outlook

Given current snowpack deficits across the majority of the Bear River Basin, water rights administration risk for the 2026 irrigation season is elevated. Users holding junior priority water rights within the Bear River system face a high likelihood of curtailment notices as the season progresses and natural flows decline from present levels.

The Bear River Compact governs interstate water apportionment among Idaho, Wyoming, and Utah, and compact administration can independently trigger curtailment conditions separate from in-state priority calls. Bear Lake County irrigators should review their water right priority dates carefully and consult with the Idaho Department of Water Resources (IDWR) regarding current basin administration status.

Users should not assume that current rising flows at the Border gauge represent a sustained abundance — the limited snowpack remaining in the basin suggests this pulse may be relatively brief. Planning for reduced allocations in July and August is prudent under present conditions.

6. Groundwater Considerations

Bear Lake County lies within the Bear River Groundwater Management Area (Bear River GWMA), designated in 2001 by the Idaho Department of Water Resources. The primary aquifer system serving Bear River valley agricultural users is the Bear River Valley alluvial aquifer.

In years when surface water availability is reduced, pressure on groundwater resources typically increases as irrigators seek supplemental supply. Users considering increased groundwater pumping should verify their groundwater rights are in good standing with IDWR before increasing withdrawal rates. Increased pumping without proper authorization can result in priority conflicts and administrative action. Contact IDWR's Eastern Regional Office for current groundwater administration guidance specific to Bear Lake County.

7. Management Recommendations

Immediate Actions (Now through May)

- Verify water right status with IDWR before committing to irrigation schedules based on normal-year assumptions

- Contact PacifiCorp and the Bear River Commission to obtain current Bear Lake storage levels — this is critical for planning late-season supply

- Monitor the Bear River at Pescadero gauge closely; if flows begin declining as snowmelt from Franklin Basin and higher-elevation stations is exhausted, prepare for curtailment conditions

Planning Actions (May through June)

- Develop a deficit irrigation plan for high-value crops, identifying which fields and crops will receive priority allocation if supply is reduced

- Coordinate with your canal company or water district on expected delivery schedules and any planned demand-sharing arrangements

- Review crop mix and planting commitments with the understanding that full-season water availability cannot be assured under current snowpack conditions

- Assess groundwater backup capacity if your operation has permitted wells, and ensure pumps and infrastructure are operational before surface water shortfalls occur

Efficiency Actions (Season-long)

8. Historical Context

The 2026 water year bears comparison to several notable low-snowpack years that serve as cautionary analogs for Bear River Basin agricultural users.

2021 brought severe drought conditions across the Mountain West, resulting in significant curtailments on multiple Idaho and Utah river systems. Agricultural producers faced forced reductions in irrigated acreage and made difficult decisions about fallowing and crop abandonment in some areas.

2015 was a historically poor snow year across much of the region, with early season warmth driving premature melt similar to conditions observed in 2026. Water managers across the Bear River system implemented emergency administrative measures, and agricultural adjustments were widespread.

1977, widely regarded as one of the most severe drought years of the 20th century in the Mountain West, required extraordinary emergency measures at both state and federal levels. Agricultural impacts were severe and long-lasting in some communities.

The current season shares characteristics with each of these analogs — particularly the early and rapid snowmelt pattern. While not every low-snowpack year produces worst-case outcomes, the 2026 season warrants serious and proactive planning at every level of agricultural operation.