Early April historically marked the peak of Cascade mountain snowpack, representing the maximum water storage before spring melting begins. Snowpack in the Cascades and Olympics serves as the Pacific Northwest's natural reservoir, storing winter precipitation and releasing it gradually through spring and summer. April 1st snowpack measurements have traditionally been used to predict summer water availability for agriculture, hydroelectric power, and municipal water supplies. However, climate change has significantly altered this pattern, with peak snowpack now often occurring in March and total accumulation declining over recent decades. Modern snowpack in the Cascades typically measures 50-70% of historical averages, with profound implications for regional water management, salmon habitat, and ecosystem health throughout the dry summer months.