Samuelsen, A. (2000). A simulation of the biological response to low-frequency physical forcing in the tropical Pacific Ocean . Master's thesis, Florida State University, Tallahassee, FL.
Samuelsen, A., & O'Brien, J. J. (2008). Wind-induced cross-shelf flux of water masses and organic matter at the Gulf of Tehuantepec. Deep Sea Research Part I: Oceanographic Research Papers , 55 (3), 221–246.
Savage, A. C., Arbic, B. K., Alford, M. H., Ansong, J. K., Farrar, J. T., Menemenlis, D., et al. (2017). Spectral decomposition of internal gravity wave sea surface height in global models. J. Geophys. Res. Oceans , 122 (10), 7803–7821.
Savage, A. C., Arbic, B. K., Alford, M. H., Ansong, J. K., Farrar, J. T., Menemenlis, D., et al. (2017). Spectral decomposition of internal gravity wave sea surface height in global models: INTERNAL GRAVITY WAVE SEA SURFACE HEIGHT. J. Geophys. Res. Oceans , 122 (10), 7803–7821.
Abstract: Two global ocean models ranging in horizontal resolution from 1/128 to 1/488 are used to study the space and time scales of sea surface height (SSH) signals associated with internal gravity waves (IGWs). Frequency-horizontal wavenumber SSH spectral densities are computed over seven regions of the world ocean from two simulations of the HYbrid Coordinate Ocean Model (HYCOM) and three simulations of the Massachusetts Institute of Technology general circulation model (MITgcm). High wavenumber, high-frequency SSH variance follows the predicted IGW linear dispersion curves. The realism of high-frequency motions (>0:87 cpd) in the models is tested through comparison of the frequency spectral density of dynamic height variance computed from the highest-resolution runs of each model (1/258 HYCOM and 1/488 MITgcm) with dynamic height variance frequency spectral density computed from nine in situ profiling instruments. These high-frequency motions are of particular interest because of their contributions to the small-scale SSH variability that will be observed on a global scale in the upcoming Surface Water and Ocean Topography (SWOT) satellite altimetry mission. The variance at supertidal frequencies can be comparable to the tidal and low-frequency variance for high wavenumbers (length scales smaller than 50 km), especially in the higher-resolution simulations. In the highest-resolution simulations, the high-frequency variance can be greater than the low-frequency variance at these scales.
Savage, A. C., Arbic, B. K., Richman, J. G., Shriver, J. F., Alford, M. H., Buijsman, M. C., et al. (2017). Frequency content of sea surface height variability from internal gravity waves to mesoscale eddies. J. Geophys. Res. Oceans , 122 (3), 2519–2538.
Schoof, J. T., Arguez, A., Brolley, J., & O'Brien, J. J. (2005). A new weather generator based on spectral properties of surface air temperatures. Agricultural and Forest Meteorology , 135 (1-4), 241–251.
Schoof, J. T., & Pryor, S. C. (2006). An evaluation of two GCMs: simulation of North American teleconnection indices and synoptic phenomena. Int. J. Climatol. , 26 (2), 267–282.
Schoof, J. T., Shin, D. W., Cocke, S., LaRow, T. E., Lim, Y. - K., & O'Brien, J. J. (2009). Dynamically and statistically downscaled seasonal temperature and precipitation hindcast ensembles for the southeastern USA. Int. J. Climatol. , 29 (2), 243–257.
Scott, J. P. (2011). An Intercomparison of Numerically Modeled Flux Data and Satellite-Derived Flux Data for Warm Seclusions . Master's thesis, Florida State University, Tallahassee, FL.
Scott, R., M. Bourassa, D. Chelton, P. Cipollini, R. Ferrari, L.-L. Fu, B., Galperin, S. Gille, H.-P. Huang, P. Klein, N. Maximenko, R. Morrow, B. Qiu, E. Rodriguez, D. Stammer, R. Tailleux, and C. Wunsch. (2010). Satellite Altimetry and Key Observations: What We've Learned, and What's Possible with New Technologies. In D. D.E. and Stammer Harrison J. Hall (Ed.), Proceedings of OceanObs'09: Sustained Ocean Observations and Information for Society (Vol. 2).
