Last Updated: January 1, 2026
In the latest observations across the nation's dams and reservoirs, a comprehensive assessment reveals a mixed landscape of water storage levels, with variances that reflect the diverse climatic conditions and water management strategies at play. Some regions are experiencing surpluses, while others face droughts, underscoring the importance of adaptive water management.
Among the reservoirs recording higher than average storage levels are Lake Almanor in California, which currently holds over a million acre-feet more than its average, signifying a surplus that benefits local ecosystems and water supply. Conversely, Lake Powell in Arizona reflects a stark deficit, with its storage levels falling approximately 8 million acre-feet short of the average, indicative of the prolonged drought affecting the Colorado River Basin. Similarly, New Mexico's Elephant Butte Reservoir storage is significantly below its historical average, echoing water scarcity concerns in the Southwest. These conditions not only impact water availability for human consumption but also have far-reaching effects on agriculture, hydroelectric power generation, and natural habitats. The variances in reservoir levels can often be traced back to factors such as snowpack levels, river flows, and regional precipitation patterns, which are influenced by broader climatic shifts and require ongoing monitoring and responsive water management strategies to ensure sustainable use and conservation of this vital resource.
Oklahoma has numerous reservoirs and dams, with the largest being Lake Texoma on the Red River. Other major reservoirs include Lake Eufaula, Lake Tenkiller, and Keystone Lake. These reservoirs are fed by various streams, rivers, and creeks, with many of them originating in the surrounding mountains of the Ozarks and Ouachitas. Snowpack is not a significant contributor to the water supply in Oklahoma, as the state typically receives little snowfall. Drought conditions are common in Oklahoma, with some reservoirs experiencing record low levels during prolonged dry spells. Seasonal trends show varying levels of precipitation and streamflow throughout the year, with the highest levels typically occurring in the spring and early summer. Overall, the hydrology of Oklahoma is heavily influenced by precipitation patterns and the unique geology of the region, with reservoirs and dams serving as crucial components of water management and conservation efforts.
Oklahoma has numerous reservoirs and dams, with the largest being Lake Texoma on the Red River. Other major reservoirs include Lake Eufaula, Lake Tenkiller, and Keystone Lake. These reservoirs are fed by various streams, rivers, and creeks, with many of them originating in the surrounding mountains of the Ozarks and Ouachitas. Snowpack is not a significant contributor to the water supply in Oklahoma, as the state typically receives little snowfall. Drought conditions are common in Oklahoma, with some reservoirs experiencing record low levels during prolonged dry spells. Seasonal trends show varying levels of precipitation and streamflow throughout the year, with the highest levels typically occurring in the spring and early summer. Overall, the hydrology of Oklahoma is heavily influenced by precipitation patterns and the unique geology of the region, with reservoirs and dams serving as crucial components of water management and conservation efforts.