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.
Zavala-Hidalgo, J., Morey, S. L., O'Brien, J. J., & Zamudio, L. (2006). On the Loop Current eddy shedding variability. Atmosfera , 19 (1), 41–48.
Morey, S. L., Zavala-Hidalgo, J., & O'Brien, J. J. (2005). The seasonal variability of continental shelf circulation in the northern and western Gulf of Mexico from a high-resolution numerical model. In W. Sturges, & A. Lugo-Fernandez (Eds.), New Developments in the Circulation of the Gulf of Mexico . Geophys. Mongr. Ser., (161).
Zavala-Hidalgo, J., Morey, S. L., & O'Brien, J. J. (2002). On the formation and interaction of cyclonic eddies with the Loop Current using NCOM and a suite of observations. MTS/IEEE Oceans 2002 Proceedings , , 1463–1466.
Morey, S. L., O'Brien, J. J., Schroeder, W. W., & Zavala-Hidalgo, J. (2002). ), Seasonal variability of the export of river discharged freshwater in the Northern gulf of Mexico. MTS/IEEE Oceans 2002 Proceedings , , 1480–1484.
Weissman, D. E., Morey, S., & Bourassa, M. (2017). Studies of the effects of rain on the performance of the SMAP radiometer surface salinity estimates and applications to remote sensing of river plumes. In IEEE International Symposium on Geoscience and Remote Sensing IGARSS (pp. 1491–1494).
Garcia-Pineda, O., MacDonald, I., Hu, C., Svejkovsky, J., Hess, M., Dukhovskoy, D., et al. (2013). Detection of Floating Oil Anomalies From the Deepwater Horizon Oil Spill With Synthetic Aperture Radar. oceanog , 26 (2).
Özgökmen, T., Chassignet, E., Dawson, C., Dukhovskoy, D., Jacobs, G., Ledwell, J., et al. (2016). Over What Area Did the Oil and Gas Spread During the 2010 Deepwater Horizon Oil Spill? Oceanog , 29 (3), 96–107.
Morey, S. L., Wienders, N., Dukhovskoy, D. S., & Bourassa, M. A. (2018). Impact of Stokes Drift on Measurements of Surface Currents from Drifters and HF Radar. In American Geophysical Union (Vol. Fall Meeting).
Abstract: Concurrent measurements by surface drifters of different configurations and HF radar reveal substantial differences in estimates of the near-surface seawater velocity. On average, speeds of small ultra-thin (5 cm) drifters are significantly greater than co-located drifters with a traditional shallow drogue design, while velocity measurements from the drogued drifters closely match HF radar velocity estimates. Analysis of directional wave spectra measurements from a nearby buoy reveals that Stokes drift accounts for much of the difference between the velocity measurements from the drogued drifters and the ultra-thin drifters, except during times of wave breaking. Under wave breaking conditions, the difference between the ultra-thin drifter velocity and the drogued drifter velocity is much less than the computed Stokes drift. The results suggest that surface currents measured by more common approaches or simulated in models may underrepresent the velocity at the very surface of the ocean that is important for determining momentum and enthalpy fluxes between the ocean and atmosphere and for estimating transport of material at the ocean surface. However, simply adding an estimate of Stokes drift may also not be an appropriate method for estimating the true surface velocity from models or measurements from drogued drifters or HF radar under all sea conditions.
Harris, R., Pollman, C., Landing, W., Morey, S., Dukhovskoy, D., & Axelrad, D. (2010). Development of a dynamic Mercury cycling model for the Gulf of Mexico. In Geochimica et Cosmochimica Acta (Vol. 74, p. A383).
