Author Title Year Publication Volume Pages Links
Smith, S. R. ; Bourassa, M. A. ; Legler, D. M. Plan for a VOS-IMET delayed mode data center at the Florida State University
2000
Hanley, D. E. ; Bourassa, M. A. ; O'Brien, J. J. ; Smith, S. R. ; Spade, E. R. The many faces of ENSO (A quantitative evaluation of ENSO indices)
2001
Bourassa, MA Shear stress model for the aqueous boundary layer near the air-sea interface
2000 Journal of Geophysical Research – Oceans 105
1167-1176
Nedbor-Gross, R. ; Dukhovskoy, D.S. ; Bourassa, M.A. ; Morey, S.L. ; Chassignet, E.P. Investigation of the Relationship Between the Yucatan Channel Transport and the Loop Current Area in a Multidecadal Numerical Simulation
2014 Marine Technology Society Journal 48
15-26
Bourassa, M. A., D. Dukhovskoy, S. L. Morey, and J, J. O'Brien Innovations in Modeling Gulf of Mexico Surface Turbulent Fluxes
2007 Flux News 9
Morey, S. ; Wienders, N. ; Dukhovskoy, D. ; Bourassa, M. Measurement Characteristics of Near-Surface Currents from Ultra-Thin Drifters, Drogued Drifters, and HF Radar
2018 Remote Sensing 10
1633
Morey, S. ; Wienders, N. ; Dukhovskoy, D. ; Bourassa, M. Measurement Characteristics of Near-Surface Currents from Ultra-Thin Drifters, Drogued Drifters, and HF Radar
2018 Remote Sensing 10
1633
Ali, M. ; Singh, N. ; Kumar, M. ; Zheng, Y. ; Bourassa, M. ; Kishtawal, C. ; Rao, C. Dominant Modes of Upper Ocean Heat Content in the North Indian Ocean
2018 Climate 6
71
Ali, M. ; Singh, N. ; Kumar, M. ; Zheng, Y. ; Bourassa, M. ; Kishtawal, C. ; Rao, C. Dominant Modes of Upper Ocean Heat Content in the North Indian Ocean
2019 Climate 6
1 – 8
Wentz, F.J. ; Ricciardulli, L. ; Rodriguez, E. ; Stiles, B.W. ; Bourassa, M.A. ; Long, D.G. ; Hoffman, R.N. ; Stoffelen, A. ; Verhoef, A. ; O'Neill, L.W. ; Farrar, J.T. ; Vandemark, D. ; Fore, A.G. ; Hristova-Veleva, S.M. ; Turk, F.J. ; Gaston, R. ; Tyler, D. Evaluating and Extending the Ocean Wind Climate Data Record
2017 IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing 10
2165-2185
