Water Intelligence Brief · Archive
August 31, 2026
Arkansas River Basin | August 31, 2026
Arkansas River flows in Otero County are at critically low late-season levels, with the Apishapa River near Fowler registering only 5 cfs (rising) and no recent data available at the La Junta and Rocky Ford gauges — conditions that signal severely constrained canal delivery capacity for Fort Lyon, Catlin, and Holbrook irrigators entering the final weeks of the irrigation season. With Fry-Ark imported water for 2026 forecasted at approximately 6,500 AF — roughly 10% of the 20-year average — this season stands as one of the most supply-constrained on record for the lower Arkansas Valley, and Rocky Ford cantaloupe, onion, alfalfa, and corn producers should treat remaining irrigation windows as a finite, depleting resource. Reservoir storage data and 7-day forecast details are available in the full brief.
Both SNOTEL stations monitoring the upper Arkansas headwaters are fully melted out as of August 30, 2026:
No percent-of-median figures are reported for either station, which is expected — the historical median SWE for this date is also 0.0", meaning these readings reflect normal seasonal conditions for late August. The accurate concern is not current snowpack deficit but meltout timing: both stations melted out approximately 4–6 weeks ahead of the historical median meltout date, driven by an anomalous March 2026 heat wave. That early meltout translated into an accelerated and compressed runoff pulse earlier in the season, with Pueblo Reservoir inflows now tapering toward base flow. No additional snowmelt contribution to downstream flows should be expected from the upper basin for the remainder of the 2026 irrigation season.
Available gauge data for the Arkansas River Basin in and near Otero County is limited, with two of three primary gauges reporting no recent data:
The 5 cfs reading on the Apishapa — a tributary system — indicates minimal late-season flow, though the rising trend warrants monitoring. The absence of current data at both the La Junta and Rocky Ford gauges is a significant operational gap. Under normal late-season conditions, the difference between the Rocky Ford gauge (which captures flow after Fort Lyon Canal diversions) and the La Junta gauge provides useful intelligence about active diversion volumes; that comparison is unavailable today. Users should contact their canal company directly for current diversion and delivery status. The data gap does not change the underlying supply picture: with Fry-Ark imports at approximately 10% of the 20-year average and the snowmelt pulse exhausted, mainstem flows are operating under severe seasonal stress.
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Data Sources: SNOTEL data through August 30, 2026; USGS streamflow data through August 31, 2026
Data Current As Of: August 31, 2026
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 Eastern Colorado Area Office (Loveland, CO — administers Fryingpan-Arkansas Project and Pueblo Reservoir), Southeastern Colorado Water Conservancy District (SECWCD), and Colorado Division of Water Resources, Water Division 2 (Pueblo office) for regulatory decisions and water rights administration. USGS gauge outages may affect completeness of streamflow analysis — verify current conditions directly with USGS National Water Information System (waterdata.usgs.gov).
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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