“…The complexity present in the ENSO impact over Europe results in part from several ENSO teleconnections that propagate through different geographical regions, as well as different atmospheric levels (Rodríguez-Fonseca et al, 2016). For example, teleconnections can propagate through the extratropical troposphere (Bulić and Kucharski, 2012;Jiménez-Esteve and Domeisen, 2018;Mezzina et al, 2020), the extratropical stratosphere (Butler et al, 2014;Ayarzagüena et al, 2018;Domeisen et al, 2019), or the Caribbean region (Wulff et al, 2017;Hardiman et al, 2019;Rieke et al, 2021). Furthermore, the ENSO teleconnection can be modulated by different regions and processes along its way, such as the tropical North Atlantic (Sung et al, 2013;Casselman et al, 2021) and the Indian Ocean (Zhong et al, 2005;Fletcher and Cassou, 2015;Joshi et al, 2021).…”