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Zavala-Hidalgo, J., Romero-Centeno, R., Mateos-Jasso, A., Morey, S. L., & Martínez-López, B. (2014). The response of the Gulf of Mexico to wind and heat flux forcing: What has been learned in recent years? Atmósfera, 27(3), 317–334.
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Harris, R., Pollman, C., Hutchinson, D., Landing, W., Axelrad, D., Morey, S. L., et al. (2012). A screening model analysis of mercury sources, fate and bioaccumulation in the Gulf of Mexico. Environ Res, 119, 53–63.
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Harris, R., Pollman, C., Landing, W., Evans, D., Axelrad, D., Hutchinson, D., et al. (2012). Mercury in the Gulf of Mexico: sources to receptors. Environ Res, 119, 42–52.
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Nedbor-Gross, R., Dukhovskoy, D. S., Bourassa, M. A., Morey, S. L., & Chassignet, E. P. (2014). Investigation of the Relationship Between the Yucatan Channel Transport and the Loop Current Area in a Multidecadal Numerical Simulation. Mar Technol Soc J, 48(4), 15–26.
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Todd, A. C., Morey, S. L., & Chassignet, E. P. (2014). Circulation and cross-shelf transport in the Florida Big Bend. J Mar Res, 72(6), 445–475.
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Hiester, H. R., Morey, S. L., Dukhovskoy, D. S., Chassignet, E. P., Kourafalou, V. H., & Hu, C. (2016). A topological approach for quantitative comparisons of ocean model fields to satellite ocean color data. Methods in Oceanography, 17, 232–250.
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Morey, S. L., & Dukhovskoy, D. S. (2013). A downscaling method for simulating deep current interactions with topography – Application to the Sigsbee Escarpment. Ocean Modelling, 69, 50–63.
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Dukhovskoy, D. S., Morey, S. L., Martin, P. J., O'Brien, J. J., & Cooper, C. (2009). Application of a vanishing, quasi-sigma, vertical coordinate for simulation of high-speed, deep currents over the Sigsbee Escarpment in the Gulf of Mexico. Ocean Modelling, 28(4), 250–265.
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Yu, P., Morey, S. L., & O'Brien, J. J. (2009). A reduced-dynamics variational approach for the assimilation of altimeter data into eddy-resolving ocean models. Ocean Modelling, 27(3-4), 215–229.
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Dukhovskoy, D. S., Morey, S. L., & O'Brien, J. J. (2006). Influence of multi-step topography on barotropic waves and consequences for numerical modeling. Ocean Modelling, 14(1-2), 45–60.
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