The Caney watershed, located in southern Kansas and northern Oklahoma, covers approximately 2,221 square miles. The hydrology of the watershed is dominated by the Caney River, which flows for 135 miles before emptying into the Verdigris River. The watershed receives an average of 38 inches of precipitation annually, with the majority falling during the summer months. The watershed also experiences occasional droughts and floods. The Caney watershed does not typically receive significant snowfall, as it is located in a relatively warm and humid region. However, occasional winter storms can bring snow and ice to the area, which can impact hydrological processes. Surface water in the Caney watershed is primarily used for agricultural and industrial purposes, with several large reservoirs providing water storage and recreation opportunities. These reservoirs can also have significant impacts on the hydrology of the watershed. Interesting climatic facts and trends in the Caney watershed include increasing temperatures and changing precipitation patterns, which can have significant impacts on water resources and ecosystems. Additionally, the watershed is located in an area prone to severe weather events such as tornadoes and thunderstorms.