Zamudio, L., Hogan, P., & Metzger, E. J. (2008). Summer generation of the Southern Gulf of California eddy train.
J. Geophys. Res., 113(C6).
Zamudio, L., Metzger, E. J., & Hogan, P. (2011). Modeling the seasonal and interannual variability of the northern Gulf of California salinity.
J. Geophys. Res., 116(C2).
Trasviña, A., Heywood, K. J., Renner, A. H. H., Thorpe, S. E., Thompson, A. F., & Zamudio, L. (2011). The impact of high-frequency current variability on dispersion off the eastern Antarctic Peninsula.
J. Geophys. Res., 116(C11).
Palacios-Hernández, E., Carrillo, L., Lavín, M. F., Zamudio, L., & García-Sandoval, A. (2006). Hydrography and circulation in the Northern Gulf of California during winter of 1994-1995.
Continental Shelf Research, 26(1), 82–103.
Zamudio, L., & Hogan, P. J. (2008). Nesting the Gulf of Mexico in Atlantic HYCOM: Oceanographic processes generated by Hurricane Ivan.
Ocean Modelling, 21(3-4), 106–125.
Zamudio, L., Metzger, E. J., & Hogan, P. J. (2010). Gulf of California response to Hurricane Juliette.
Ocean Modelling, 33(1-2), 20–32.
Buijsman, M. C., Arbic, B. K., Richman, J. G., Shriver, J. F., Wallcraft, A. J., & Zamudio, L. (2017). Semidiurnal internal tide incoherence in the equatorial Pacific.
J. Geophys. Res. Oceans, 12(7), 5286–5305.
Allende-Arandía, M. E., Zavala-Hidalgo, J., Romero-Centeno, R., Mateos-Jasso, A., Vargas-Hernández, J. M., & Zamudio, L. (2016). Analysis of Ocean Current Observations in the Northern Veracruz Coral Reef System, Mexico: 2007-12.
Journal of Coastal Research, 317, 46–55.
Shinoda, T., Han, W., Zamudio, L., Lien, R. - C., & Katsumata, M. (2017). Remote Ocean Response to the Madden-Julian Oscillation during the DYNAMO Field Campaign: Impact on Somali Current System and the Seychelles-Chagos Thermocline Ridge.
Atmosphere, 8(9), 171.
Adams, D. K., McGillicuddy, D. J. J., Zamudio, L., Thurnherr, A. M., Liang, X., Rouxel, O., et al. (2011). Surface-generated mesoscale eddies transport deep-sea products from hydrothermal vents.
Science, 332(6029), 580–583.
Abstract: Atmospheric forcing, which is known to have a strong influence on surface ocean dynamics and production, is typically not considered in studies of the deep sea. Our observations and models demonstrate an unexpected influence of surface-generated mesoscale eddies in the transport of hydrothermal vent efflux and of vent larvae away from the northern East Pacific Rise. Transport by these deep-reaching eddies provides a mechanism for spreading the hydrothermal chemical and heat flux into the deep-ocean interior and for dispersing propagules hundreds of kilometers between isolated and ephemeral communities. Because the eddies interacting with the East Pacific Rise are formed seasonally and are sensitive to phenomena such as El Nino, they have the potential to introduce seasonal to interannual atmospheric variations into the deep sea.