Model engine: mpi-Princeton Ocean Model – 3D currents, T/S, SSH, turbulence KE (TKE) & length w/wave- breaking and Stokes drift TKE production; wave- enhanced BBL; 4 th -order pressure grad scheme; Grids: horizontal: 3~5km, vertical: 25 levels; Topography: Etopo2+NOS digitized map on shelves; Open Transport and climatological T/S + radiation [Oey & Chen, 1992a,b; JGR]; Surface fluxes: CCMP wind ( ); NCEP/GFS 2010-present; supplemented w/hurricane winds from AOML’s HRD; Heat & salt fluxes: monthly climatology or daily NCEP; 51 Rivers: daily, 34 in GOM, 17 east coast; Data assimilation: SSHA, SST, Drifters, bred-ensemble; Tides: M2, S2, K1 & O1; Wind-waves: yes, w/option to couple with currents; Inundation: yes; Nesting: yes (not used here, but see publications). Figure Caption: mpiPOM model domain of the northwestern Atlantic Ocean including the Gulf of Mexico & Caribbean Sea. Color is sea-surface height (SSH; in meters) on Jun/19/2010 – red indicates high SSH = 0.5m, and blue is low SSH = -0.5m. Squiggly black lines indicate the corresponding surface currents velocity in m/s (2 scales are shown for water depths deeper and shallower than 200m). Blue vectors indicate kinematic wind stress vectors in (m/s) 2 (i.e. wind stress in N/m 2 divided by water density ~ 1000 kg/m 3 ). Grey contour is the 50m isobath, and white contour is 200m. Princeton’s Circulation & Wave Model of the Northwestern Atlantic Ocean (

25. Xu & Oey, 2011: The origin of the along-shelf pressure gradient in the Mid-Atlantic Bight, J. Phys. Oceanogr. In press. 24. Chang, Oey, Xu, Lu & Fujisaki, 2011: 2010 Oil Spill - trajectory projections based on ensemble drifter analyses. Ocn Dyn, DOI: /s Chang & Oey, 2011: Loop Current Cycle. J. Phys. Oceanogr., 41, Chang & Oey, 2010: Eddy and wind-forced heat transports in the Gulf of Mexico. J. Phys. Oceanogr. 40, Chang & Oey, 2010: Why can wind delay the shedding of Loop Current eddies? J. Phys. Oceanogr., 40, Oey, Chang, Sun & Lin, 2009: Topocaustics. Ocean Modelling, 29, Oey, Inoue, Lai, Lin, Welsh & Rouse Jr. 2008: Stalling of near-inertial waves in a cyclone. GRL, 35, L12604, doi: /2008GL Oey, 2008: Loop Current and Deep Eddies. J. Phys. Oceanogr. 38, Mellor, Donelan, Oey, 2008: A Surface Wave Model for Coupling with Numerical Ocean Circulation Models. J. Atmos. Oceanic Tech, 25, Wang & Oey, 2008: Hindcast of Waves and Currents in Hurricane Katrina. Bulletin of the American Meteorological Society (BAMS), April, Oey, Ezer, Wang, Yin and Fan, 2007: Hurricane-induced motions and interaction with ocean currents, CSR, doi: /j.csr Yin & Oey, 2007: Bred-ensemble ocean forecast of Loop Current and rings, Ocean Modelling, doi: /j.ocemod Lin, Oey & Wang, 2007: Altimetry and drifter assimilations of Loop Current and eddies. JGR, 112, C05046, doi: /2006JC003779, Oey, Ezer, Wang, Fan & Yin, 2006: Loop current warming by Hurricane Wilma. GRL, 33, L08613, doi: /2006GL Oey, Ezer, Forristall, Cooper, DiMarco & Fan, 2005: An exercise in forecasting loop current and eddy frontal positions in the Gulf of Mexico. Geophysical Research Letters, 32, L12611, doi: /2005GL Oey, L.-Y., T. Ezer and H.-C. Lee, 2005: Loop Current, rings and related circulation in the Gulf of Mexico: A review of numerical models and future challenges. In, Circulation in the Gulf of Mexico: Observations and Models, W. Sturges and A. Lugo-Fernandez (Eds.), Geophys. Monograph Ser., Vol. 161, American Geophysical Union, Washington, DC, Schmitz, Biggs, Lugo-Fernandez, Oey and Sturges, A synopsis of the circulation in the Gulf of Mexico and on its continental margins. In: Circulation in the Gulf of Mexico: Observations and Models, W. Sturges and A. Lugo-Fernandez, editors, AGU Geophysical Monograph 161, Fan, S., L-Y. Oey, and P. Hamilton, 2004: Assimilation of drifter and satellite data in a model of the Northeastern Gulf of Mexico. CSR, 24(9), Oey, L-Y., 2004: Vorticity flux through the Yucatan Channel and Loop Current variability in the Gulf of Mexico. JGR, 109, C10004, doi: /2004JC Oey, L-Y., T. Ezer, and W. Sturges, 2004: Modeled and observed empirical orthogonal functions of currents in the Yucatan Channel, Gulf of Mexico. Journal of Geophysical Research, 109(C08011), doi: /2004JC Oey & Zhang, 2004: The generation of subsurface cyclones and jets through eddy-slope interaction. Continental Shelf Research, 24(18), Ezer, T., L-Y. Oey, and H-C. Lee, and W. Sturges, 2003: The variability of currents in the Yucatan Channel: Analysis of results from a numerical ocean model. Journal of Geophysical Research, 108(C1), 3012, /2002JC Oey, L-Y., H-C. Lee, and W. J. Schmitz, Jr., 2003: Effects of winds and Caribbean eddies on the frequency of Loop Current eddy shedding: A numerical model study. J Geophys Res, 108(C10), 3324, doi: /2002JC Wang, D-P., L-Y. Oey, T. Ezer, and P. Hamilton, 2003: Near-surface currents in DeSoto Canyon (1997–99): Comparison of current meters, satellite observation, and model simulation. Journal of Physical Oceanography, 33(1), Oey, L.-Y., and H. C. Lee, 2002: Deep eddy energy and topographic Rossby waves in the Gulf of Mexico. J Phys Oceanogr, 32(12), PROFS references (since 2002, model-related and Western Atlantic only)

Apr/01~Aug/31/2010 Animation (daily) of model SSH (color) + surface currents (white squiggly vectors) and observed drifters (black squiggly vectors) Date SSH (m) 0.2 m/s 200m 2000m The Loop Current X MC252