OS31C:
Ocean Submesoscale Processes and Potential Scientific Breakthrough: Simulations, Observations, and Applications I Posters

Wednesday, 17 December 2014: 8:00 AM-12:20 PM
Chairs:  Tamay M Ozgokmen, University of Miami, Miami, FL, United States and Yann Drillet, Mercator Océan, Ramonville-Saint-Agne, France
Primary Convener:  Patrice Klein, IFREMER, LPO, Plouzané, France
Co-conveners:  Bo Qiu, Univ Hawaii Manoa, Honolulu, HI, United States, Jorge Vazquez, NASA Jet Propulsion Laboratory, Pasadena, CA, United States and Mike Chin, Jet Propulsion Laboratory, Pasadena, CA, United States

Abstracts Submitted to this Session:

1000
 
Importance of 3D Processes Near the Ocean’s Surface for Material Transport
Tamay M Ozgokmen, University of Miami, Miami, FL, United States
1001
 
Characteristics and Seasonality of the Submesoscale Regime in the Gulf Stream Region
Jean Alberto Mensa1, Zulema D Garraffo2, Annalisa Griffa3, Tamay M Ozgokmen1, Angelique C Haza4 and Carmela Veneziani5, (1)University of Miami, Miami, FL, United States, (2)NOAA/EMC--IMSG Scientist III, College Park, MD, United States, (3)ISMAR, CNR, Lerici, Italy, (4)University of Miami, Ocean Sciences, Miami, FL, United States, (5)Los Alamos National Laboratory, Fluid Dynamics and Solid Mechanics, Division T-3 MSB216, Los Alamos, NM, United States
1002
 
Gulf Stream Slope Eddies and their Submesocale Interior
Jonathan Gula, Maarten J Molemaker and James C McWilliams, University of California Los Angeles, Los Angeles, CA, United States
1003
 
A Description of Local and Nonlocal Eddy-Mean Flow Interaction in a Global Eddying State Estimate
Carl I Wunsch1,2, Ru Chen3 and Glenn Flierl1, (1)Massachusetts Institute of Technology, Cambridge, MA, United States, (2)Harvard University, Cambridge, MA, United States, (3)Scripps Institution of Oceanography, La Jolla, CA, United States
1004
 
Bjerknes-like Compensation Between Eddy Components of Meridional Heat Transport in the Wintertime North Pacific
Stuart P Bishop, Frank Bryan and R. Justin Small, National Center for Atmospheric Research, Boulder, CO, United States
1005
 
Toward Submesocale Ocean Modelling and Observations for Global Ocean Forecast.
Yann Drillet, Mercator Océan, Ramonville-Saint-Agne, France
1006
 
Resonant generation and energetics of wind-forced near-inertial motions in a submesoscale jet
Daniel B Whitt and Leif N Thomas, Stanford University, Stanford, CA, United States
1007
 
Mixed Layer Formation and Restratification in the Presence of Mesoscale and Submesoscale Turbulence
Xavier Couvelard1, Anne Marie Tréguier2, Franck Dumas1, Valérie Garnier1 and Aurelien Ponte2, (1)IFREMER, Dyneco/Physed, Plouzané, France, (2)IFREMER, LPO, Plouzané, France
1008
 
Surprisingly low near-inertial energy flux leaving the ocean’s mixed layer
Antonija Rimac1, Jin-Song von Storch1 and Carsten Eden2, (1)Max Planck Institute for Meteorology, Ocean, Hamburg, Germany, (2)University of Hamburg, Hamburg, Germany
1009
 
Damping of Balanced Motions during Critical Reflection of Inertial Waves Off the Sea Surface at Ocean Fronts
Nicolas Grisouard, Stanford University, Los Altos Hills, CA, United States and Leif N Thomas, Stanford University, Stanford, CA, United States
1010
 
Impact of Submesoscale Eddies on Synoptic and Mesoscale Oceanic Structures in a Continental Shelf Margin Analyzed with a Downscaling Ocean Model of Japan Sea
Dai Miyazaki1, Yusuke Uchiyama1, Ryosuke Kanki1 and Yasumasa Miyazawa2, (1)Kobe University, Kobe, Japan, (2)JAMSTEC, Yokohama, Japan
1011
 
Estimating the Numerical Diapycnal Mixing in the GO5.0 Ocean Model
Alex Megann and George Nurser, National Oceanography Center, Soton, Southampton, United Kingdom
1012
 
The seasonal evolution of submesoscale turbulence statistics from an O(1 km)-resolving mooring array
Christian Buckingham1, Liam Brannigan2, Alberto Naveira Garabato3, Andrew F Thompson4, Ayah Lazar4, George Nurser5 and David Philip Marshall2, (1)University of Southampton, National Oceanography Centre, Southampton, United Kingdom, (2)University of Oxford, Physics, Oxford, United Kingdom, (3)University of Southampton, National Oceanography Centre, Southampton, SO14, United Kingdom, (4)California Institute of Technology, Pasadena, CA, United States, (5)National Oceanography Center, Soton, Southampton, United Kingdom
1013
 
Year-long observations of open-ocean submesoscale motions from ocean gliders
Andrew F Thompson1, Ayah Lazar1, Gillian Damerell2, Karen J Heywood3, Christian Buckingham4, Alberto Naveira Garabato5 and Liam Brannigan6, (1)California Institute of Technology, Pasadena, CA, United States, (2)University of East Anglia, Norwich, United Kingdom, (3)University of East Anglia, Norwich, NR4, United Kingdom, (4)University of Southampton, National Oceanography Centre, Southampton, United Kingdom, (5)University of Southampton, National Oceanography Centre, Southampton, SO14, United Kingdom, (6)University of Oxford, Physics, Oxford, United Kingdom
1014
 
Sub-mesoscale Circulation in the Southern Ocean
Isabella Rosso, Australian National University, Canberra, ACT, Australia, Andrew Hogg, Australian National University, Canberra, Australia, Peter G Strutton, University of Tasmania, Hobart, TAS, Australia, Andrew E Kiss, University of New South Wales Canberra at the Australian Defence Force Academy, Canberra, Australia and Richard Matear, CSIRO Hobart, Hobart, Australia
1015
 
Response of phytoplankton to submesoscale dynamics in the western North Pacific
Yoshikazu Sasai1, Hideharu Sasaki1, Patrice Klein2 and Bo Qiu3, (1)JAMSTEC, Yokohama, Japan, (2)IFREMER, LPO, Plouzané, France, (3)Univ Hawaii Manoa, Honolulu, HI, United States
1016
 
The Importance of Submesoscale Versus Basin-scale Processes in Driving the Subpolar Spring Phytoplankton Bloom.
Sarah Brody, Duke University, Earth and Ocean Sciences, Durham, NC, United States, Amala Mahadevan, Woods Hole Oceanographic Institution, Woods Hole, MA, United States and M. Susan Lozier, Duke University, Durham, NC, United States
 
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