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Early Snowpack Peak and Dry Soils Impact Utah Water Runoff

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A macro view of dry, cracked Utah soil meeting a small remnant of melting snow, symbolizing the disconnect between early snowpack and thirsty ground during the spring thaw in Utah's mountainside landscape.
Photo via AI illustration
Utah's snowpack peaked ten days earlier than usual this year, while record-dry soils have impacted runoff efficiency for streams, rivers, and lakes.

Key takeaways

  • Snowpack peaked ten days earlier than usual this year.
  • Record-dry soils are reducing runoff efficiency into streams, rivers, and lakes.
  • Soil moisture levels are at their lowest since 2006 monitoring began.
  • All 29 Utah counties are experiencing some level of drought.
  • Low soil moisture means ground will absorb precipitation before it can reach reservoirs.

The Utah Division of Water Resources reports that the state's snowpack reached its peak ten days early this year. This early peak, combined with record-dry soils, has decreased the efficiency of runoff that typically fills the state's lakes, rivers, and streams.

Record dry weather in 2020 marked the eighth warmest calendar year on record. Current soil moisture levels have reached their lowest points since monitoring began in 2006.

Because of these low moisture levels, the ground is expected to soak up precipitation first, which reduces the amount of runoff available to fill reservoirs and streams.

All 29 counties in Utah are currently experiencing some level of drought. While agencies continue to monitor water levels closely to react to changing conditions, officials noted that opportunities exist to decrease water use through aggressive conservation efforts.

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