Is the Atlantic Ocean playing an increasingly important role in El Niño events? This research explores how Atlantic warming enhances the influence of the Atlantic Niño on the El Niño–Southern Oscillation (ENSO). The purpose of this study was to investigate the impact that ESL students' level of English Language Proficiency had on their level of academic motivation. The results suggest that the warmer background of the tropical Atlantic plays an essential role in enhancing local mean precipitation, inducing stronger divergence and low‐level easterlies in the Pacific. Through model pacemaker experiments, the study probes the relative contributions of changes in the Atlantic Niño and the mean-state under global warming. Under a favorable condition in the Pacific, even a weak Atlantic Niño‐related warming could promote the development of La Niña through cross‐basin Walker circulation and the Indian Ocean‐relayed Kelvin wave response. The results suggest that the warmer background of the tropical Atlantic plays an essential role in enhancing local mean precipitation, inducing stronger divergence and low‐level easterlies in the Pacific. In contrast, the Atlantic Niño pattern change itself induces feeble convection anomalies in the western Atlantic, which cannot induce significant atmospheric response in the Pacific. These results imply an important modulation of global warming on the inter-basin connection. These results imply an important modulation of global warming on the inter‐basin connection. The warmer background of the tropical Atlantic plays an essential role in enhancing local mean precipitation, inducing stronger divergence and low‐level easterlies in the Pacific.
This research is relevant to Geophysical Research Letters, given its focus on climate patterns and ocean-atmosphere interactions. By examining the influence of Atlantic warming on ENSO, it contributes to understanding global climate dynamics. This research is advancing atmospheric science through data analysis.