OKLAHOMA RESERVOIR REPORT

Last Updated: February 11, 2026

Across the nation, dams and reservoirs play a crucial role in water supply, agricultural irrigation, flood control, and recreation. Currently, there is a notable variance in storage levels, reflecting diverse hydrological conditions. For instance, Lake Powell, straddling Arizona, exhibits storage levels significantly below average, with current storage at 6,058,625 acre-ft compared to the historical average of 14,671,042.6 acre-ft, indicating potential water supply stress and hydroelectric power generation challenges. In contrast, Utah Lake in Utah is experiencing a surplus, with storage levels rising to 690,563 acre-ft from the average of 629,839.45 acre-ft. These variations are indicative of broader environmental patterns, such as precipitation, snowpack conditions, and river flows that feed into these critical water bodies.

On a more granular level, California's Lake Almanor and Lake San Antonio are above their historical storage averages, possibly a result of targeted conservation measures and above-average precipitation. Conversely, Colorado's Dillon, Granby, and Green Mountain reservoirs are all reporting storage below average, which may raise concerns about water availability for the upcoming dry season. Similarly, New Mexico's Heron and El Vado reservoirs are well below their average storage levels, pointing to ongoing drought conditions that could affect local water restrictions and management decisions. As hydrologists and water management experts continue to monitor these vital resources, the data underscores the importance of adaptive water management strategies to navigate the variability and challenges posed by changing climatic conditions.

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.