Obey

Watershed Hydrology

The Obey Watershed, also known as HUC 05130105, covers an area of approximately 300 square miles in Tennessee and Kentucky. The headwaters of the watershed originate in the Cumberland Plateau and flow into the Obey River, which eventually empties into the Cumberland River. The watershed is characterized by a humid subtropical climate with hot summers and mild winters. The area receives an average of 50 inches of precipitation annually, with the majority falling in the form of rain during the summer months. The watershed is also home to the Dale Hollow Reservoir, which was created by the construction of the Dale Hollow Dam in 1943. The reservoir is used for hydroelectric power generation, flood control, and recreation. The reservoir is fed by the Obey River and its tributaries, and is known for its excellent fishing opportunities. The watershed is subject to significant snowfall during the winter months, which can impact surface water flow and reservoir levels. In recent years, the area has experienced warming temperatures and reduced snowfall, which has led to concerns about water availability and impacts on the local ecosystem.


Surface Flows

Obey Watershed

Snowpack Depths

Obey Watershed

Dams & Reservoirs

Obey Watershed

Groundwater Levels

Obey Watershed

Obey Rivers

Rivers of the Watershed