- Record February snow at Alta highlights potential for ample spring runoff.
- Statewide snowpack above normal, boosting Utah’s water position.
- Soils are saturated, promising good streamflow and reservoir refill.
- Great Salt Lake sees significant rise, aided by conservation efforts.
- Full reservoirs underscore the importance of water infrastructure.
March 12, 2024 — According to a report from the Utah Department of Natural Resources, Utah’s water situation is looking good this March. A record-breaking February snowfall at Alta highlights how quickly things can improve and bodes well for the upcoming spring runoff season. Across the state, snowpack levels are significantly above average, putting Utah’s water supply in a healthy position.
The Natural Resources Conservation Service report paints a reassuring picture with the state’s snow water equivalent (SWE) showing a 157% increase over typical amounts for February. This translates to a statewide SWE at 117% of normal. Importantly, soil moisture levels are high, meaning much of the melting snow will make its way directly into streams and reservoirs rather than being absorbed by dry ground. These factors set the stage for a strong spring runoff season.
Reservoirs are already reaping the benefits, sitting at an impressive 83% capacity – drastically higher than the previous year’s levels. These ‘water savings accounts’ demonstrate the power of infrastructure in securing the state’s water resources.
The Great Salt Lake, a major focus of conservation efforts, has also shown a significant rise in water levels (1.8 feet since October). Actions like modifying the GSL berm aid salinity management and benefit the lake’s ecosystem.
While the current outlook is encouraging, Utah officials warn that it is crucial to remain vigilant about water conservation. Programs like the Agricultural Optimization Program and SlowtheFlow.org foster water-wise practices to ensure Utah’s water resilience for years.
Image:
Adams Canyon, Layton, Utah. Jacques Demien, October 2019, public domain via Wikimedia Commons.
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