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Xu, X., Bower, A., Furey, H., & Chassignet, E. P. (2018). Variability of the Iceland-Scotland Overflow Water Transport Through the Charlie-Gibbs Fracture Zone: Results From an Eddying Simulation and Observations. J. Geophys. Res. Oceans, (8).
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Kranz, S. A., Wang, S., Kelly, T. B., Stukel, M. R., Goericke, R., Landry, M. R., et al. (2020). Lagrangian Studies of Marine Production: A Multimethod Assessment of Productivity Relationships in the California Current Ecosystem Upwelling Region. J. Geophys. Res. Oceans, 125(6).
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Bourassa, M. A. (2000). Shear stress model for the aqueous boundary layer near the air-sea interface. Journal of Geophysical Research – Oceans, 105(C1), 1167–1176.
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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.
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Spiesberger, J. L., Hurlburt, H. E., Johnson, M., Keller, M., Meyers, S., & O'Brien, J. (1998). Acoustic thermometry data compared with two ocean models: the importance of Rossby waves and ENSO in modifying the ocean interior. Dynamics of Atmospheres and Oceans, 26(4), 209–240.
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Misra, V., Mishra, A., & Li, H. (2016). The sensitivity of the regional coupled ocean-atmosphere simulations over the Intra-Americas seas to the prescribed bathymetry. Dynamics of Atmospheres and Oceans, 76, 29–51.
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Dukhovskoy, D., & Bourassa, M. (2011). Comparison of ocean surface wind products in the perspective of ocean modeling of the Nordic Seas. In OCEANS 2011.
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Morey, S. L., & Dukhovskoy, D. S. (2011). A Multi-Model Nesting Approach for Simulating Deep Ocean Dynamics and Topographic Interactions. In OCEANS 2011.
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Weissman, D. E., H. Winterbottom, and M. A. Bourassa. (2010). The influence of rainfall upon scatterometer estimates for sea surface stress: applications to boundary layer parameterization and drag coefficient models within tropical cyclone environments. In OCEANS 2010, MTS/IEEE (pp. 1–7).
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Kvaleberg, E., Morey, S. L., & O'Brien, J. J. (2003). Frontogenesis and subsequent formation of cold filaments and eddies on an idealized shelf. In OCEANS 2003 MTS/IEEE: Celebrating the Past... Teaming toward the Future (pp. 2831–2834).
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