A recent study in Nature highlights the increasing frequency and severity of summer streamflow droughts in western Canadian watersheds, focusing on the Fraser and upper Columbia Basins. The research identifies reduced snowpack, warmer temperatures, and lower precipitation levels as primary drivers. The drought events of 2023 and 2024 were influenced by varying combinations of these factors, underscoring the complex interplay between snowpack, temperature, and precipitation in determining drought intensity. The research also investigates the role of ENSO in influencing drought conditions, emphasizing the importance of understanding this climate pattern for improved drought forecasting and preparedness.