The heavy snowfall that has blanketed Utah throughout the winter may be rapidly leading to major flooding, as the state’s water resources department forecasts a heightened risk of floods in the coming months.
The U.S. Department of Agriculture’s Natural Resources Conservation Service (NRCS) has recently determined that the snowpack in Utah is at a record-breaking level, and it is not expected to decrease significantly anytime soon. As a result, the NRCS has warned that the state is inching closer to major flooding.
The snowpack, which is the water stored in the snow, is currently at more than 160% of normal, with more than 200% in the northern part of the state. This has caused the snowpack to exceed the capacity of the state’s water resources, leading to a greater risk of flooding.
The NRCS has projected that the snowpack in Utah will remain above normal through April, which is typically the peak of the snowpack season. This means that the snowpack will likely remain above normal until the summer months, when it is expected to decrease.
The high snowpack levels have also increased the amount of water that is flowing into the state’s reservoirs. This has caused the reservoirs to become full, which has put a strain on their capacity to hold water.
If the snowpack continues to remain at high levels or increases, the state could see an increase in flooding. This could cause significant damage to homes and businesses, as well as impact the state’s infrastructure.
The NRCS has suggested that the state take steps to reduce the risk of flooding, such as releasing more water from the reservoirs, building additional reservoirs, or improving drainage systems. The state has also begun to implement measures to reduce the risk of flooding, such as installing flood gates to protect vulnerable areas.
While the snowpack levels are expected to decrease by the summer, the NRCS has warned that the state should remain vigilant. As the snowpack continues to remain at record-breaking levels, Utah may be inching closer to major flooding.