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Dukhovskoy, D. S., Morey, S. L., & O'Brien, J. J. (2005). Topographic Rossby Waves in a Z-Level Ocean Model (J. Cote, Ed.). Research Activities in Atmospheric and Ocean Modeling, Report No. 35. Geneva, Switzerland: World Meteorological Organization.
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Dukhovskoy, D. S., Morey, S. L., & O'Brien, J. J. (2005). Topographic Rossby waves in a z-level ocean model. Eos Trans. AGU, 86(18), Jt. Assem. Suppl., Abstract OS22A–06.
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Dukhovskoy, D. S., Morey, S. L., & O'Brien, J. J. (2006). Baroclinic topographic waves on the Nicaragua Shelf generated by tropical cyclones (J. Cote, Ed.). Research Activities in Atmospheric and Ocean Modeling, Report No. 36. Geneva, Switzerland: World Meteorological Organization.
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Gouillon, F., Dukhovskoy, D. D., Morey, S. L., & O'Brien, J. J. (2006). Modeling tides in a semi-enclosed basin: A case study of the Gulf of Mexico (J. Cote, Ed.). Research Activities in Atmospheric and Ocean Modeling, Report No. 36. Geneva, Switzerland,: World Meteorological Organization.
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Henson, J. I., Muller-Karger, F., Wilson, D., Morey, S. L., Maul, G. A., Luther, M., et al. (2006). Strategic geographic positioning of sea level gauges to aid in early detection of tsunamis in the Intra-Americas Sea. Science of Tsunami Hazards, 25(3), 173–207.
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Kvaleberg, E., Morey, S. L., & O'Brien, J. J. Modeling frontal instabilities in the Gulf of Mexico (J. Cote, Ed.). Research Activities in Atmospheric and Ocean Modeling, Report No. 33. Geneva, Switzerland: World Meteorological Organization.
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Kvaleberg, E., Morey, S. L., & O'Brien, J. J. (2004). (J. Cote, Ed.). Research Activities in Atmospheric and Ocean Modeling, Report No. 34. Geneva, Switzerland: World Meteorological Organization.
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Morey, S. L. (1997). The effects of Halmahera on the Indonesian overflow. Master's thesis, Florida State University, Tallahassee, FL.
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Morey, S. L. (1999). The spring transition of thermal stratification on a mid-latitude continental shelf. Ph.D. thesis, Florida State University, Tallahassee, FL.
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Morey, S. L. (2012). Spatial variability of upwelling on a continental shelf inferred from satellite scatterometry. In IEEE International Symposium on Geoscience and Remote Sensing IGARSS (pp. 7094–7097).
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