What Makes an El Niño "Super"?
El Niño events arise from prolonged, anomalously warm equatorial Pacific sea surface temperatures (>2.0°C anomaly). In winter, this shifts the Pacific jet stream southward, funneling intense atmospheric river (AR) plumes directly into California and the West Coast, causing high-volume continuous precipitation events.
Atmospheric River Categorization
The Ralph et al. AR scale rates storm plumes from Category 1 (primarily beneficial) to Category 5 (predominantly hazardous). Super El Niño seasons often trigger back-to-back Category 4 and 5 systems that leave zero drying time between rainfall surges, inducing saturated soil failures.
Critical Safety Measures
Turn around, don't drown: 6 inches of moving water can knock down an adult, and 12 inches can sweep away small cars. Sign up for county Nixle and Everbridge emergency alerts, keep NOAA weather radio operational, and prepare evacuation paths away from canyon mouths.