Award Abstract # 0550227
Collaborative Research: Does Topography Control Mesocale Dissipation?

NSF Org: OCE
Division Of Ocean Sciences
Recipient: UNIVERSITY OF CALIFORNIA, LOS ANGELES
Initial Amendment Date: March 31, 2006
Latest Amendment Date: March 31, 2006
Award Number: 0550227
Award Instrument: Standard Grant
Program Manager: Eric C. Itsweire
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: April 1, 2006
End Date: March 31, 2010 (Estimated)
Total Intended Award Amount: $222,982.00
Total Awarded Amount to Date: $222,982.00
Funds Obligated to Date: FY 2006 = $222,982.00
History of Investigator:
  • James McWilliams (Principal Investigator)
    jcm@atmos.ucla.edu
  • Jeroen Molemaker (Co-Principal Investigator)
Recipient Sponsored Research Office: University of California-Los Angeles
10889 WILSHIRE BLVD STE 700
LOS ANGELES
CA  US  90024-4200
(310)794-0102
Sponsor Congressional District: 36
Primary Place of Performance: University of California-Los Angeles
10889 WILSHIRE BLVD STE 700
LOS ANGELES
CA  US  90024-4200
Primary Place of Performance
Congressional District:
36
Unique Entity Identifier (UEI): RN64EPNH8JC6
Parent UEI:
NSF Program(s): PHYSICAL OCEANOGRAPHY
Primary Program Source: app-0106 
Program Reference Code(s): 0000, OTHR
Program Element Code(s): 161000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

The turbulent mechanical energy budget of the subsurface ocean has recently received considerable attention because it is key to understanding the global conveyor circulation. However, there exists a dissipation crisis in the mechanical energy budget. Energy is fed to the system and then dissipated by invoking eddy viscosities (the forms and values for which are dictated first and foremost by computational stability constraints). Essential oceanographic measures, like eddy kinetic energy, are determined by these parameterizations, and the implications of mesoscale dissipation are far reaching. This includes including diapycnal heat and tracer fluxes. To help clarify the issues surrounding the limitations of mesoscale energy loss, the parameterizations need to be developed from physical approaches and model calculations.

In this study, researchers at the University of Rhode Island, Florida State University, and the University of California at Los Angeles will compute the energy losses to boundary dissipation, topographically induced unbalanced flows, and internal mesoscale dissipative mechanisms resulting from a topographically forced forward energy cascade to smaller scales. The team of scientists will conduct and analyze fine resolution primitive equation and non-hydrostatic model simulations of interactions of vortices and seamounts as a prototype for topographically induced loss-of-balance and dissipation. The principal tools will be analytical and process numerical models. The results gathered from this work will comment on the viability of their hypothesis that the interaction between the mesoscale and topography is important in controlling the mesoscale, principally through catalyzing transfers from balanced to unbalanced currents. If true, this information will impact the ocean sub-grid scale parameterization, from bottom boundary layers to interior mixing. In addition to the intellectual merit of the work, the research will train a graduate student and promote cooperation between scientists at URI, FSU, and UCLA. The results will be refereed to journals and presented at national and international scientific meetings and in seminars.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Capet, X., J.C. McWilliams, M.J. Molemaker, and A.F. Shchepetkin "Mesoscale to submesoscale transition in the California Current System: Energy balance and flux" J. Phys. Ocean. , v.38 , 2008 , p.2256
Capet, X., J.C. McWilliams, M.J. Molemaker, and A.F. Shchepetkin "Mesoscale to submesoscale transition in the California Current System: Flow Structure, eddy flux and osbservational tests" J. Phys. Ocean. , v.38 , 2008 , p.29
Capet, X., J.C. McWilliams, M.J. Molemaker, and A.F. Shchepetkin "Mesoscale to submesoscale transition in the California Current System: Frontal Processes" J. Phys. Ocean. , v.38 , 2008 , p.44
Capet, X., J.C. McWilliams, M.J. Molemaker, and A.F. Shchepetkin "Mesoscale to submesoscale transition in the California Current System: Part I: Flow Structure and eddy flux" J. Phys. Ocean. , v.38 , 2008 , p.29
Capet, X., J.C. McWilliams, M.J. Molemaker, and A.F. Shchepetkin "Mesoscale to submesoscale transition in the California Current System: Part II: Dynamical processes and observational tests" J. Phys. Ocean. , v.38 , 2008 , p.44
Ferrari, R., and J.C. McWilliams, "Parameterization of eddy fluxes near oceanic boundaries" J. Climate , v.21 , 2008 , p.2770
McWilliams, J.C, F. Colas, and M.J. Molemaker "Cold Filamentary intensification and oceanic surface convergence lines" Geosphys. Res. Lett. , v.36 , 2009 , p.L18602 10.1029/2009GL039402
McWilliams, J.C, M.J. Molemaker, and E.I. Olafsdottir "Linear fluctuation growth during frontogenesis" J. Phys. Ocean , v.39 , 2009 , p.3111
Molemaker, M.J., and J.C. McWilliams "Local balance and crossscale" J. Fluid Mech. , v.645 , 2010 , p.295
Molemaker, M.J., J.C. McWilliams, and X. Capet "Balanced and unbalanced routes to dissipation in an equilibrated Eady flow" J. Fluid Mech. , v.654 , 2010 , p.35

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