Understanding the physical controls on tropical cyclone (TC) frequency represents a major challenge, as there is no theory to explain why the global annual number of TCs is relatively constant in historical observations and no consensus on future changes in TC frequency (Sobel et al., 2021). Pre-existing low-pressure disturbances, or TC "seeds," may trigger TC genesis, and have been identified as one possible factor in determining TC frequency. The typical Atlantic TC seed is provided by African easterly waves (AEWs), which are synoptic-scale disturbances that grow off of the baroclinic and barotropic instability of the African easterly jet (AEJ) (Burpee, 1972). AEWs generate between 5°N and 30°N over tropical northern Africa (Kiladis et al., 2006) and propagate westward over the tropical Atlantic Ocean.There is a strong connection between AEWs and Atlantic TCs on the synoptic time scale (Dieng et al., 2017;Landsea et al., 1998), with about 60%-80% of major Atlantic hurricanes originating from AEWs (Landsea, 1993;Russell et al., 2017). However, some studies have suggested that the relationship between TC frequency and AEWs may not be as straightforward as previously thought, especially on climate time scales. For instance, results from Hodges (2001) andHopsch et al. (2007) suggest that the relationship between AEWs and Atlantic TC activity could depend on the period considered, with the former finding them to be correlated for one period whereas the latter found them to be uncorrelated for a different period using the same data product. Moreover, Thorncroft and Hodges (2001) showed that only AEWs leaving the West African coast with significant low-level amplitudes, rather than the total number of AEWs, may influence the seasonal Atlantic