“…The intensity and extension of the currents change at seasonal and inter-annual scales and numerous sub-mesoscale and mesoscale features facilitate recirculation, settlement of larvae close to their spawning sites, and larval exchange with neighboring jurisdictions (Paris and Cowen, 2004;Paris et al, 2005;Kough et al, 2013;Kough et al, 2016;Lopera et al, 2020). Indeed, numerous recurrent gyres are known to occur in the region, notably the semi-permanent cyclonic Panama-Colombia Gyre (Lopera et al, 2020), the transient Honduras and Cozumel Gyres (Carrillo et al, 2015), and the anti-cyclonic gyre around Cayman Islands (Molinari, 1980). Thus, differences in connectivity between the hydrodynamic products reflect the variability of these surface and subsurface flow patterns, particularly around the Lesser and Greater Antilles, which affect the connectivity patterns between The Bahamas, Cuba, and the Windward and Leeward Islands.…”