The KRWMP is a critical component of Oklahoma City’s long-term water supply strategy. It supports the growing needs of more than 1.5 million people throughout Central Oklahoma who rely on Oklahoma City for water. Today, raw water is sourced from four primary reservoirs that span nearly 250 miles across the state: Lakes Hefner and Stanley Draper in Oklahoma City, Canton Reservoir in northwest Oklahoma, and Atoka and McGee Creek Reservoirs in southeast Oklahoma.
This regional approach is guided by a comprehensive lake management plan that balances use across all supply reservoirs to promote sustainability and reliability.
Some local community members have raised questions about why Oklahoma City doesn’t rely more heavily on nearby aquifers, and the answer lies in both history and science. From Oklahoma City's founding through the late 1990s, groundwater wells were used alongside surface water from the North Canadian River system. During the drought of record in the 1950s, the City ramped up groundwater use in a desperate attempt to supplement Lakes Overholser and Hefner—but many wells dried up within days. A 1954 study concluded that groundwater could not serve as a sustainable long-range water supply, prompting the City to pursue more reliable surface water sources in southeast Oklahoma.
Subsequent studies confirmed that conclusion. A 2014 report by the U.S. Geological Survey and Oklahoma Water Resources Board found the Garber-Wellington Aquifer, which lies beneath the Oklahoma City metro, to be unreliable and declining in yield. As a result, it is not considered a sustainable water source for a large metropolitan area.
To ensure a safe, sustainable, and resilient water future, Oklahoma City has strategically invested in surface water infrastructure. The KRWMP builds on that plan, preparing the region to meet future demand while protecting water quality and public health for Oklahoma City as well as for Oklahomans who reside within the Kiamichi River Basin, and all basins from which the City receives water.