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Subtropical Jet Wave Train Associated With North Atlantic SST Contributes to ENSO‐Like Anomalies

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The anticyclonic anomaly over the eastern tropical Pacific promotes unusual atmospheric conditions, enhancing atmospheric convection and precipitation.
A positive sea surface temperature gradient in the northeastern Atlantic induces a significant precipitation anomaly by creating a cyclonic anomaly.
This observational analysis highlights how subtropical jet wave trains contribute to global climatic patterns through remote SST influences.
The findings suggest that changes in North Atlantic SST could have far-reaching effects on the development of ENSO-like anomalies.

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Observational analysis shows that subtropical jet influences ENSO-related climate anomalies, suggesting potential interactions with SST.

An et al. (2025) studied this question.

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