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Elsner, J. B., Strazzo, S. E., Jagger, T. H., LaRow, T., & Zhao, M. (2013). Sensitivity of Limiting Hurricane Intensity to SST in the Atlantic from Observations and GCMs. J. Climate, 26(16), 5949–5957.
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De Souza-Machado, S., Tangborn, A., Sura, P., Hepplewhite, C., & Strow, L. L. (2017). Non-Gaussian Analysis of Observations from the Atmospheric Infrared Sounder Compared with ERA and MERRA Reanalyses. J. Appl. Meteor. Climatol., 56(5), 1463–1481.
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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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Nyadjro, E. S., Jensen, T. G., Richman, J. G., & Shriver, J. F. (2017). On the Relationship Between Wind, SST, and the Thermocline in the Seychelles-Chagos Thermocline Ridge. IEEE Geosci. Remote Sensing Lett., 14(12), 2315–2319.
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Li, H., Kanamitsu, M., & Hong, S. - Y. (2012). California reanalysis downscaling at 10 km using an ocean-atmosphere coupled regional model system. J. Geophys. Res., 117(D12).
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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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Boisserie, M., Shin, D. W., LaRow, T. E., & Cocke, S. (2006). Evaluation of soil moisture in the Florida State University climate model-National Center for Atmospheric Research community land model (FSU-CLM) using two reanalyses (R2 and ERA40) and in situ observations. J. Geophys. Res., 111(D8).
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Roads, J. (2003). International Research Institute/Applied Research Centers (IRI/ARCs) regional model intercomparison over South America. J. Geophys. Res., 108(D14).
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Morey, S. L. (2002). The spring transition from horizontal to vertical thermal stratification on a midlatitude continental shelf. J. Geophys. Res., 107(C8).
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Misra, V., Mishra, A., & Bhardwaj, A. (2017). High-resolution regional-coupled ocean-atmosphere simulation of the Indian Summer Monsoon. Int. J. Climatol, 37, 717–740.
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