
NSF Org: |
OCE Division Of Ocean Sciences |
Recipient: |
|
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: |
|
History of Investigator: |
|
Recipient Sponsored Research Office: |
10889 WILSHIRE BLVD STE 700 LOS ANGELES CA US 90024-4200 (310)794-0102 |
Sponsor Congressional District: |
|
Primary Place of Performance: |
10889 WILSHIRE BLVD STE 700 LOS ANGELES CA US 90024-4200 |
Primary Place of
Performance Congressional District: |
|
Unique Entity Identifier (UEI): |
|
Parent UEI: |
|
NSF Program(s): | PHYSICAL OCEANOGRAPHY |
Primary Program Source: |
|
Program Reference Code(s): |
|
Program Element Code(s): |
|
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
Note:
When clicking on a Digital Object Identifier (DOI) number, you will be taken to an external
site maintained by the publisher. Some full text articles may not yet be available without a
charge during the embargo (administrative interval).
Some links on this page may take you to non-federal websites. Their policies may differ from
this site.
Please report errors in award information by writing to: awardsearch@nsf.gov.