Colorado's mountain snowpack has reached its lowest level since statewide recordkeeping began in 1941 [1].
The depletion of this critical water source threatens the state's long-term water security and increases the risk of wildfires during the summer months. Because the mountains act as a natural reservoir, the lack of snow reduces the gradual release of water into streams and reservoirs.
Maureen Gutsch, a hydrologist at Colorado State University, confirmed the severity of the situation. "Colorado just had its worst snowpack since statewide recordkeeping began in 1941," Gutsch said [1].
The crisis affects several regions, including the Front Range and the San Juan Mountains [2]. Experts attribute the depletion to a combination of record-low snowfall, a persistent drought across the western U.S., and broader climate-change trends [1, 3].
Some reports describe the snowpack as essentially gone, leaving the state with only a fraction of the water it typically relies on [4]. While some areas experienced late-season weather events, these did not reverse the trend. For example, a winter storm warning in May predicted 14 inches of snow for the mountains [5].
Alex Lehnert of CBS News Colorado noted that the overall snowpack remained historically low despite those recent additions. "Even with the recent snowfall, the overall snowpack remains historically low," Lehnert said [6].
The current conditions create a volatile environment for the coming months. Dry vegetation and low soil moisture, products of the missing snowpack, provide fuel for wildfires that can spread more rapidly across the landscape [3].
“"Colorado just had its worst snowpack since statewide recordkeeping began in 1941."”
The collapse of the 2026 snowpack represents a critical failure of the state's primary water storage system. This creates a compounding disaster: immediate water shortages for agriculture and municipal use, paired with an elevated wildfire risk due to desiccated forests. The fact that this is the worst level in 85 years suggests that traditional water management strategies may no longer be sufficient to combat the effects of long-term regional drought and climate shifts.
