Increasingly variable hydrologic regimes combined with more frequent and intense extreme events are challenging water management, emphasizing the need for accurate medium- to long-term predictions to timely prompt anticipatory operations. Modern forecasts are becoming increasingly skillful over short lead times, but predictability generally decreases at longer lead times. Global climate teleconnections, such as El Niño Southern Oscillation (ENSO) and North Atlantic Oscillation (NAO), may contribute to extending forecast lead times. However, the contribution of ENSO states to local predictability depends on the degree to which local conditions are affected by this climate state. This teleconnection is well defined in some locations, such as ...