A harsh winter has struck the western United States, leaving many mountainous regions with critically low snowpack levels. This phenomenon, known as a snow drought, is attributed to warmer-than-average temperatures and increased precipitation falling as rain rather than snow.
According to satellite images from NASA's Terra satellite, on January 15, only 142,700 square miles (369,700 square kilometers) of the western U.S. were blanketed with snow, marking the lowest coverage for that date in over two decades. The region has seen above-average precipitation in recent months, but record warmth has resulted in much of it falling as rain instead of snow.
The National Integrated Drought Information System reports that the snow drought is most acute in Washington, Oregon, Colorado, Utah, Arizona, and New Mexico. In some areas, snow water equivalent β a measure of the amount of water stored in the snowpack β is at its lowest levels in at least 20 years.
Climate scientist Daniel Swain attributes the snow deficit to temperature-driven changes, stating that "this is a classic climate-change, temperature-driven, elevationally dependent snowpack deficit." He notes that while high-elevation areas have seen more precipitation as snow, this has not been enough to make up for deficits lower in the mountains.
The health of the mountain snowpack is crucial for ecosystems, wildfire dynamics, and water availability during drier times of the year. However, with significant amounts of winter still remaining, it remains uncertain whether snowfall in coming months will be able to mitigate existing deficits. In regions already dry, such as the Pacific Northwest and the Colorado River Basin, the impact may be exacerbated rather than alleviated.
NASA's Earth Observatory provides satellite images of the situation, including a chart showing that January 2026 snow coverage was significantly below the January median, as well as the previous minimum from 2015.
According to satellite images from NASA's Terra satellite, on January 15, only 142,700 square miles (369,700 square kilometers) of the western U.S. were blanketed with snow, marking the lowest coverage for that date in over two decades. The region has seen above-average precipitation in recent months, but record warmth has resulted in much of it falling as rain instead of snow.
The National Integrated Drought Information System reports that the snow drought is most acute in Washington, Oregon, Colorado, Utah, Arizona, and New Mexico. In some areas, snow water equivalent β a measure of the amount of water stored in the snowpack β is at its lowest levels in at least 20 years.
Climate scientist Daniel Swain attributes the snow deficit to temperature-driven changes, stating that "this is a classic climate-change, temperature-driven, elevationally dependent snowpack deficit." He notes that while high-elevation areas have seen more precipitation as snow, this has not been enough to make up for deficits lower in the mountains.
The health of the mountain snowpack is crucial for ecosystems, wildfire dynamics, and water availability during drier times of the year. However, with significant amounts of winter still remaining, it remains uncertain whether snowfall in coming months will be able to mitigate existing deficits. In regions already dry, such as the Pacific Northwest and the Colorado River Basin, the impact may be exacerbated rather than alleviated.
NASA's Earth Observatory provides satellite images of the situation, including a chart showing that January 2026 snow coverage was significantly below the January median, as well as the previous minimum from 2015.