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Metzger, E. J., H.E. Hurlburt, A.J. Wallcraft, O.M. Smedstad, J.A. Cummings, and E.P. Chassignet. (2009). Predicting Ocean Weather using the HYbrid Coordinate Ocean Model (HYCOM). NRL Review, , submitted.
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Timko, P. G., Arbic, B. K., Richman, J. G., Scott, R. B., Metzger, E. J., & Wallcraft, A. J. (2013). Skill testing a three-dimensional global tide model to historical current meter records. J. Geophys. Res. Oceans, 118(12), 6914–6933.
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Xu, X., Chassignet, E. P., Johns, W. E., Schmitz Jr, W. J., & Metzger, E. J. (2014). Intraseasonal to interannual variability of the Atlantic meridional overturning circulation from eddy-resolving simulations and observations. J. Geophys. Res. Oceans, 119(8), 5140–5159.
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Zamudio, L., Hurlburt, H. E., Metzger, E. J., & Smedstad, O. M. (2002). On the evolution of coastally trapped waves generated by Hurricane Juliette along the Mexican West Coast. Geophys. Res. Lett., 29(23), 56–1-56–4.
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Zamudio, L., Hurlburt, H. E., Metzger, E. J., Morey, S. L., O'Brien, J. J., Tilburg, C., et al. (2006). Interannual variability of Tehuantepec eddies. J. Geophys. Res., 111(C5).
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Kara, A. B., Metzger, E. J., & Bourassa, M. A. (2007). Ocean current and wave effects on wind stress drag coefficient over the global ocean. Geophys. Res. Lett., 34(1).
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Zamudio, L., Hurlburt, H. E., Metzger, E. J., & Tilburg, C. E. (2007). Tropical wave-induced oceanic eddies at Cabo Corrientes and the María Islands, Mexico. J. Geophys. Res., 112(C5).
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Zamudio, L., Hogan, P., & Metzger, E. J. (2008). Summer generation of the Southern Gulf of California eddy train. J. Geophys. Res., 113(C6).
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Kara, A. B., Metzger, E. J., Hurlburt, H. E., Wallcraft, A. J., & Chassignet, E. P. (2008). Multistatistics metric evaluation of ocean general circulation model sea surface temperature: Application to 0.08° Pacific Hybrid Coordinate Ocean Model simulations. J. Geophys. Res., 113(C12).
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Arbic, B. K., Shriver, J. F., Hogan, P. J., Hurlburt, H. E., McClean, J. L., Metzger, E. J., et al. (2009). Estimates of bottom flows and bottom boundary layer dissipation of the oceanic general circulation from global high-resolution models. J. Geophys. Res., 114(C2).
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