11/14/2024, 5:38 am EST
Likely related to latent heat release of late season tropical cyclones in both the North Atlantic and Northwest Pacific, a gathering of anomalous warm air aloft leading to a high-pressure block convenes over Greenland characteristic of a strong negative phase North Atlantic oscillation. In the middle latitudes, compensating cold trough patterns develop and replace the prevailing very warm climate of autumn 2024.