Award Abstract # 1355970
Dynamical and Material Connectivity Across Continental Shelves

NSF Org: OCE
Division Of Ocean Sciences
Recipient: UNIVERSITY OF CALIFORNIA, LOS ANGELES
Initial Amendment Date: January 24, 2014
Latest Amendment Date: January 24, 2014
Award Number: 1355970
Award Instrument: Standard Grant
Program Manager: Baris Uz
bmuz@nsf.gov
 (703)292-4557
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: February 1, 2014
End Date: January 31, 2018 (Estimated)
Total Intended Award Amount: $631,905.00
Total Awarded Amount to Date: $631,905.00
Funds Obligated to Date: FY 2014 = $631,905.00
History of Investigator:
  • James McWilliams (Principal Investigator)
    jcm@atmos.ucla.edu
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
CA  US  90095-1567
Primary Place of Performance
Congressional District:
36
Unique Entity Identifier (UEI): RN64EPNH8JC6
Parent UEI:
NSF Program(s): PHYSICAL OCEANOGRAPHY
Primary Program Source: 01001415DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s):
Program Element Code(s): 161000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Inside the surf zone, the water is typically well mixed because wave action dominates dynamics and creates strong turbulence. Further offshore on the continental shelf, the water is stratified by density and circulation is primarily driven by wind and by pressure gradients. These two regimes are typically studied separately because of the drastic differences in the dynamics and scales of variability. However, exchange processes at the Surf-Shelf Transition Zone (SSTZ) are critical for a number of important concerns ranging from larval transport to pollution. This study will develop and use modeling approaches that handle both sets of dynamics and scales gracefully and lead to a better understanding of this important transition zone.


The primary hypotheses are (1) the SSTZ has high intrinsic variability beyond the wind-, tide- and wave-forced flows; (2) surf eddies and submesoscale shelf eddies have intermittent strong interactions; and (3) the eddies play a dominant role in setting the rates of material transport across and along bathymetric gradients, as well as vertically through the pycnocline. This research program is a necessary precursor to addressing the many important fluxes of biogeochemical, ecological, pollutant, and sedimentary fluxes within the SSTZ. The approach is to use a multiply-nested circulation model (Regional Oceanic Modeling System, ROMS) that includes the wave-averaged Stokes drift vortex force and material advection and wave-augmented mixing processes, coupled to a surface gravity wave model that includes Doppler-shift refraction by the current. It will be used for a set of idealized SSTZ process studies to assess the competing influences of bathymetric shape; stratification; surface waves; prevailing alongshore currents and their instability; surf eddies; shelf eddies and coastally-trapped waves; tides; and storm-water inflows. In addition, realistic ROMS simulations, with full physics and aggressive down-scale grid nesting, will be made for extensive periods at several SSTZ sites in Southern California, and existing measurements will provide model validation tests. Realistic SSTZ modeling and validation studies will be extended to other sites through unpaid collaborations with Japanese and Santa Barbara colleagues.

Intellectual Merit :
Both surf eddies and submesoscale shelf eddies are relatively unexplored phenomena, and the proposed comprehensive theoretical and computational examination of their nature, dynamics, and material transport effects in the SSTZ will lead to new phenomenological discoveries, future field experiments for validation, and reassessments of the material fluxes in this front-line human-ocean interface.

Broader Impacts :
The nearshore region is the primary intersection of human activities with the ocean, and progress in understanding and modeling its behavior for currents, pollutants, ecosystems, inundation, and beach morphology will empower better management and protection. The knowledge gained will be disseminated through professional and public lectures and publications; by consultation with National Weather Service beach safety forecasters and Orange County, CA, wastewater managers; and by inclusion into the undergraduate and graduate ocean curriculum at UCLA. It will provide research training for a minority STEM graduate student. Its research collaborations will strengthen both an international scientific cooperation with Japan and the physical oceanographic underpinnings of the Long Term Ecological Research program on the giant kelp forest ecosystem in the Santa Barbara Channel.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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(Showing: 1 - 10 of 26)
Akan, C., J.C. McWilliams, H.T. Ozkan-Haller, and S. Moghimi "Frontal dynamics at the mouth of the Columbia River" Ocean Modelling , v.122 , 2017 , p.1
Ardhuin, F., N. Suzuki, J.C. McWilliams, and H. Aiki "Commentson ``A Combined Derivation of the Integrated and Vertically Resolved,Coupled Wave-Current Equations''" J. Phys. Ocean. , v.47 , 2017 , p.2377
Barkan, R., J.C. McWilliams, A.F. Shchepetkin, M.J. Molemaker, L. Renault, A. Bracco, and J. Choi "Submesoscale dynamics in the northern Gulf of Mexico. Part I: Regional and seasonal characterization and the role of rivers" J. Phys. Ocean. , v.47 , 2016 , p.2325
Barkan, R., J.C. McWilliams, M.J. Molemaker, A.F. Shchepetkin, K. Srinivasan, J. Choi, and A. Bracco "Submesoscale dynamics in the northern Gulf of Mexico. Part II: Temperature-salinity relations and cross-shelf transport processes" J. Phys. Ocean. , v.47 , 2017 , p.2347
Choi, J., A. Bracco, R. Barkan, A.F. Shchepetkin, and J.C. McWilliams "Submesoscale dynamics in the northern Gulf of Mexico. Part III: Lagrangian implications" J. Phys. Ocean. , v.47 , 2017
Dauhajre, D., & J.C. McWilliams "Submesoscale fronts in the inner contintenal shelf" J. Phys. Ocean. , v.47 , 2017 , p.2949
Kumar, N., F. Feddersen, S. Sutara, Y. Uchiyama, and J.C. McWilliams "Mid- to inner-shelf coupled ROMS-SWAN model-data comparison ofcurrents and temperature: Dirunal and semi-diurnalvariability" J. Phys. Ocea , v.46 , 2017 , p.862
Kumar, N., F. Feddersen, S. Sutara, Y. Uchiyama, and J.C. McWilliams "Mid- to inner-shelf coupled ROMS-SWAN model-data comparison of waves, currents, and temperature: Dirunal and semi-dirunal variability" J. Phys. Ocean. , v.45 , 2016 , p.841
Kumar, N., F. Feddersen, Y. Uchiyama, J.C. McWilliams, andA.F. Shchepetkin "Mid-shelf to surf zone coupled ROMS-SWAN modeldata comparison of waves, currents, and temperature" Ocean Modelling , v.45 , 2015 , p.1464
Kumar, N., F. Feddersen, Y. Uchiyama, J.C. McWilliams, and W. O'Reilly "Mid-shelf to surf zone coupled ROMS-SWAN model data comparison of waves, currents, and temperature: Diagnosis of subtidal forcings" J. Phys. Ocean. , v.45 , 2015 , p.1464
Kumar, N., F. Feddersen, Y. Uchiyama, J. McWilliams, & W. O'Reilly "Mid-shelf tosurf zone coupled ROMS-SWAN model-data comparison of waves, currents, and temperature:Diagnosis of subtidal forcings and response" J. Phys. Ocean. , v.45 , 2015 , p.1464
(Showing: 1 - 10 of 26)

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

The shallower margins of the ocean have atypical currents,specifically the wind-driven flows on the continental shelf and thewave-driven currents in the adjacent surf zone where incident surfacegravity waves break and disappear near the shoreline.  Both of thesephenomena are at first understood in terms of their wind or waveforcing cause, but they also develop spontaneous variations becausethe directly forced currents are unstable.  The ensuing "turbulence"of shelf and surf currents is usually the more important experience ofmariners and swimmers than are the more systematic direct flows.Furthermore, the trajectories of floating or dissolved materials areusually quite irregular and chaotic.  This project has investigatedthe nature of shelf and surf turbulence, how these two types of flowsare related to each other, and how materials are moved betweenshallower and deeper waters.  The scientific approach is to firstmathematically derive a theory for how the waves influence currents,mainly through the so-called Stokes drift they induce in the water,and then to solve a computational model for the ensuing currents underthe combined influences of the wind, wave breaking, and Stokes drift.The simulations show previously unexpected behaviors of recirculatingeddies, both within the surf zone and occasionally drifting furtheroffshore, and of sharp "fronts" outside the surf zone with largechanges in water density and temperature across them and strongcurrents along them.  This has led to a better understanding of whatthe fluctuating currents are and what their added influence is ondispersal of materials in this region of the ocean.  Besides thesescientific discoveries, the technical capability for realisticsimulation modeling of shelf and surf currents has been improved.These outcomes are useful in guiding rescue operations (rip currents),pollution management, and commercial and recreational fisheries incoastal waters.


Last Modified: 02/12/2018
Modified by: James C Mcwilliams

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