Speleothems are cave minerals that preserve signals of past climate in their geochemical composition. In the western United States (US), speleothem-based climate reconstructions can provide valuable insight into the long-term evolution of modern drought patterns that impact agriculture, ecosystems, and human communities today. The El Niño Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO) are key drivers of cool-season precipitation variability and drought in the western US, including the Rocky Mountains.
