Utah drought Eases to two-thirds of state as El Niño brings rain

Utah drought Eases to two-thirds of state as El Niño brings rain

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A State Soaked: Utah’s Drought Eases, but at a Cost

Less than two weeks ago, over 90% of Utah was locked in some form of drought. On Thursday, that number had plummeted to two-thirds. KSL reported this dramatic shift, driven by an atmospheric river of rain tied to the El Niño pattern. The change isn’t just a line on a map; it’s a transformation felt in saturated soil, swelling reservoirs, and the urgent calls for rescues as waterways overflowed their banks.

This deluge, which dumped 7.4 trillion gallons of water on the state from September 1 to November 3, has pulled significant portions of Utah out of the most severe drought classifications. For the first time since June 2025, parts of the Uintas range and southeast Utah are no longer listed in any drought category at all. “We’re kind of in uncharted territory,” said Jordan Clayton, a hydrologist for the Natural Resources Conservation Service and director of the Utah Snow Survey, highlighting the sheer scale of the moisture.

The Numbers Behind the Shift

The data from the U.S. Drought Monitor tells a story of rapid improvement. While two-thirds of the state still faces dry conditions, the nature of that dryness has changed dramatically. Severe or extreme drought, which gripped over half the state just last week, now covers only about 36%. The most significant improvements are in southern Utah, where a large chunk of the state has dropped to “abnormally dry,” the category between drought and normal.

Utah drought Eases to two-thirds of state as El Niño brings rain

The 60-day precipitation totals are staggering. Brad Pugh, a drought meteorologist with the National Weather Service’s Climate Prediction Center, noted that much of Utah, along with parts of Arizona, southern Nevada, and southern California, has seen precipitation between 200% and 400% of normal. “Precipitation amounts of more than 1 inch prompted a one-category improvement from Arizona north to Nevada, Utah and southeastern Idaho,” Pugh wrote in a report. This influx ended short-term drought conditions for the Southwest and Great Basin, though a long-term deficit persists.

“We’re kind of in uncharted territory,” said Jordan Clayton, a hydrologist for the Natural Resources Conservation Service and director of the Utah Snow Survey.

The same weather event that is replenishing Utah’s critical water supply is also causing dangerous flooding. Southern Utah has seen severe flooding, and landslides have been reported across various regions. Emergency services were stretched thin, with two people rescued after their vehicle got stuck in water released from Gunlock Reservoir, which surged from 37% capacity to over 100% in a single week.

Reservoirs Rise but Still Lag Behind

The impact on reservoirs, a vital component of the state’s water infrastructure, has been profound and, in some cases, historic. The surge at Gunlock Reservoir is just one example. Lake Powell, a key reservoir for the entire Colorado River system, has gained 17 feet in elevation over the past month. Typically, such gains are reserved for the spring snowmelt, making the recent run of moisture all the more impressive.

Yet, for all the recent good news, a sobering reality remains. Utah’s collective reservoir system is only at 50% capacity. That’s 10 percentage points below this time last year and 6 points below the median average. This lingering deficit points to the deep, long-term nature of the drought that has plagued the region. While the skies have opened up, the ground has been parched for so long that it will take more than a few weeks of rain to fully recover the long-term water debt.

Reservoir levels are just one element of the complex equation the U.S. Drought Monitor uses to classify conditions. Other impacts from the record-low snowpack of the previous year still factor into why so much of the state remains in drought.

Moisture Boosts Future Water Supply

The massive influx of moisture has a silver lining for the future. Strong soil moisture levels are directly associated with better snowpack runoff conditions in the spring. When the snow eventually melts, it will run off into streams and reservoirs more efficiently, rather than being absorbed by bone-dry earth.

The soil moisture levels have jumped to nearly 78% saturation, surpassing the median average peak during the spring snowmelt—a figure so high it has no modern precedent in the 20-year history of the soil moisture network.

The weather pattern is also expected to shift. Chilly and drier conditions are forecast for this weekend and early next week, which will likely bring soil moisture percentages back down to more typical fall levels. But long-range models suggest the active weather pattern could resume toward the middle of the month. The question now is how much more moisture that will bring, and whether it will be enough to chip away at the remaining drought in the central and northwestern sections of the state, where the worst conditions persist.

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