Author Title Year Publication Volume Pages Links
Grant, J ; Erlebacher, G ; O'Brien, J Case study: Visualizing ocean flow vertical motions using Lagrangian-Eulerian time surfaces
2002 IEEE Visualization 2002 Conference 529-532
Meyers, S.D. ; Melsom, A. ; Mitchum, G.T. ; O'Brien, J.J. Detection of the fast Kelvin wave teleconnection due to El Niño-Southern Oscillation
1998 Journal of Geophysical Research: Oceans 103
27655-27663
Latif, M. ; Anderson, D. ; Barnett, T. ; Cane, M. ; Kleeman, R. ; Leetmaa, A. ; O'Brien, J. ; Rosati, A. ; Schneider, E. A review of the predictability and prediction of ENSO
1998 Journal of Geophysical Research: Oceans 103
14375-14393
Bourassa, M.A. ; Freilich, M.H. ; Legler, D.M. ; Liu, W.T. ; O'Brien, J.J. Wind observations from new satellite and research vessels agree
1997 Eos, Transactions American Geophysical Union 78
597
Meyers, S.D. ; O'Brien, J.J. Pacific Ocean influences atmospheric carbon dioxide
1995 Eos, Transactions American Geophysical Union 76
533-533
Misra, V. ; Moeller, L. ; Stefanova, L. ; Chan, S. ; O'Brien, J.J. ; Smith III, T.J. ; Plant, N. The influence of the Atlantic Warm Pool on the Florida panhandle sea breeze: FLORIDA SEA BREEZE VARIATIONS
2011 Journal of Geophysical Research: Atmospheres 116
Gouillon, F. ; Morey, S.L. ; Dukhovskoy, D.S. ; O'Brien, J.J. Forced tidal response in the Gulf of Mexico
2010 Journal of Geophysical Research 115
Goto-Maeda, Y. ; Shin, D.W. ; O'Brien, J.J. Freeze probability of Florida in a regional climate model and climate indices
2008 Geophysical Research Letters 35
Lim, Y.-K. ; Shin, D.W. ; Cocke, S. ; LaRow, T.E. ; Schoof, J.T. ; O'Brien, J.J. ; Chassignet, E.P. Dynamically and statistically downscaled seasonal simulations of maximum surface air temperature over the southeastern United States
2007 Journal of Geophysical Research 112
Kennedy, A.J. ; Griffin, M.L. ; Morey, S.L. ; Smith, S.R. ; O'Brien, J.J. Effects of El Niño-Southern Oscillation on sea level anomalies along the Gulf of Mexico coast
2007 Journal of Geophysical Research 112
