Understanding Potential Factors Influencing the ITF in the 21 st Century Tony Lee NASA Jet Propulsion Laboratory California Institute of Technology.
Tanuja Nigam Supervisor- Dr. Vimlesh Pant Indian Institute of Technology Delhi, New Delhi Coastal Upwelling Features over Arabian Sea From ROMS-Model.
Preliminary results on Formation and variability of North Atlantic sea surface salinity maximum in a global GCM Tangdong Qu International Pacific Research.
1 Evaluation of two global HYCOM 1/12º hindcasts in the Mediterranean Sea Cedric Sommen 1 In collaboration with Alexandra Bozec 2 and Eric Chassignet 2.
WAVES AND SEA-AIR FLUXES. CALM CONDITIONS Surface waves are the most obvious feature of the ocean. They result from the density discontinuity (we have.
Using IOOS to Improve Water Quality Management in LIS James O’Donnell Frank Bohlen, Hans Dam and Grant McCardell.
Typical Mean Dynamic Balances in Estuaries Along-Estuary Component 1. Barotropic pressure gradient vs. friction Steady state, linear motion, no rotation,
Chukchi/Beaufort Seas Surface Wind Climatology, Variability, and Extremes from Reanalysis Data: 1979- 2009 Xiangdong Zhang, Jeremy Krieger, Paula Moreira,
Estimating the contribution of wind-waves in the coupled climate system WEALTH FROM OCEANS NATIONAL RESEARCH FLAGSHIP Mark Hemer 1, Baylor Fox-Kemper 2,
R. A. Brown 2003 U. ConcepciÓn. UW; Patoux, ‘03 R. A. Brown 2003 U. Concepci Ó n.
Ocean Stratification and Circulation Martin Visbeck DEES, Lamont-Doherty Earth Observatory [email protected].
State and Parameter Estimation for a Coupled Ocean-Atmosphere Model Michael Ghil Ecole Normale Supérieure, Paris, and University of California, Los Angeles.
