Text S2.
The ocean currents plus 2% windage cLCS pointing towards the coast discussed in section 3.2.3, are shown here to direct pathways of particles toward the Mexican coast in August 2018 (Figure S6). As trajectories get closer to the coast, another strong cLCS parallel to the coast redirects trajectories along the coast toward the north. Trajectory data was produced by Lara-Hernández et al. (2023) using instantaneous velocity (not the same velocity as the cLCS) plus 2% windage. Similar results hold for other months (not shown).