Acknowledgments
This study was funded by UNAM-DGAPA PAPIIT Projects TA100420 and
IA101122 and CONACYT Project 320563. Funding for the development of
HyCOM has been provided by the National Ocean Partnership Program and
the Office of Naval Research. Data assimilative products using HyCOM are
funded by the US Navy. We also thank the Ocean-Atmosphere Interaction
group of the Institute of Atmospheric Sciences and Climate Change of
UNAM for the particle transport model provided, particularly Dr. J.
Zavala-Hidalgo, as well as G.U. Martín-Ruiz and A. Ramírez-Manguilar for
IT support. Computer time was made available by the DoD High-Performance
Computing Modernization Program. RD would like to thank Julio
Lara-Hernández for the trajectory data used in Text S2. This work was
conducted under the Advanced Offshore Research Portfolio, FWP Number
1022409 at National Energy Technology Laboratory, U.S. Dept. of Energy.