Blanca Ayarzagüena

Apr 9, 2024 | rmets.onlinelibrary.wiley.com | Christopher O'Reilly |Marie Drouard |Blanca Ayarzagüena |John Methven

1 INTRODUCTION The El Niño–Southern Oscillation (ENSO) phenomenon is characterised by coupled ocean–atmosphere variability in the Tropical Pacific but has remote influences across the globe, through atmospheric teleconnections (e.g., Horel & Wallace, 1981; Trenberth et al., 1998; Wallace & Gutzler, 1981).