Decadal‐to‐centennial‐scale climate variability: Insights into the rise and fall of the Great Salt Lake

Abstract
We demonstrate connections between decadal and secular global climatic variations, and historical variations in the volume of the Great Salt Lake. The decadal variations correspond to a low‐frequency shifting of storm tracks which influence winter precipitation and explain nearly 18% of the interannual and longer‐term variance in the record of monthly volume change. The secular trend accounts for a more modest ∼1.5% of the variance.