“…However, it can also influence the subseasonal timescale through its impact on the MJO (Hendon et al., 1999; Kessler, 2001; Pohl & Matthews, 2007) and the basic state in which MJO teleconnections propagate (Moon et al., 2011; Namias, 1986; Takahashi & Shirooka, 2014), ultimately impacting the MJO's influence in the midlatitudes (Arcodia et al., 2020; Henderson & Maloney, 2018; Stan et al., 2017; Tseng et al., 2020) and subsequent subseasonal prediction skill (Johnson et al, 2014; L. Wang & Robertson, 2019). Further, recent work suggests ENSO may play a main role in changes to midlatitude subseasonal predictability in a future, warmer climate (Mayer & Barnes, 2022). While ENSO is often used for seasonal prediction (e.g., Gibson et al., 2021; Winkler et al., 2001), there is also considerable literature that highlights ENSO teleconnections as a driver of midlatitude subseasonal variability, particularly in boreal winter by also modulating the Aleutian Low (e.g., Chapman et al., 2021; Kumar & Hoerling, 1998).…”