Diagnostic of the diurnal cycle of turbulence of the Equatorial Atlantic Ocean upper boundary layer

Abstract

This work is an attempt to diagnose the turbu-lence field of the equatorial Atlantic Ocean dur-ing the dry period when the mixed layer is more highly developed using the General Ocean Turbulence Model (GOTM). A relaxation scheme assimilates the vertical profiles of in situ ob-servations (current velocity, sea temperature and salinity) during simulations. In the absence of direct turbulence observations and modeling studies of the equatorial Atlantic Ocean, the results are compared qualitatively to observed and simulated results for the equatorial Pacific Ocean. Similarities are noted between the At-lantic simulation and previous studies per-formed in the Pacific Ocean. The mechanism of nocturnal turbulence production, namely deep- cycle turbulence, is well captured by GOTM si-mulations. This deep nocturnal turbulence ap-pears rather suddenly during the night in the simulations and consequently seems to be un-related to surface wind and radiation forcing.

Share and Cite:

Skielka, U. , Soares, J. , Oliveira, A. and Servain, J. (2011) Diagnostic of the diurnal cycle of turbulence of the Equatorial Atlantic Ocean upper boundary layer. Natural Science, 3, 444-455. doi: 10.4236/ns.2011.36061.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] Thorpe, S.A. (2004) Recent development in the study of ocean turbulence. Annual Review of Earth and Planetary Sciences, 32, 91-109. doi:10.1146/annurev.earth.32.071603.152635
[2] Moum, J.N. and Caldwell, D.R. (1985) Local influences on the shear-flow turbulence in the equatorial ocean, Science, 230, 315-316. doi:10.1126/science.230.4723.315
[3] Gregg, M.C., Peters, H., Wesson, J.C., Oakey, N.S and Shay, T.J. (1985) Intensive measurements of turbulence and shear in the equatorial undercurrent. Nature, 318,140-144. doi:10.1038/318140a0
[4] Wang, D., Large, W.G. and McWilliams, J.C. (1996) Large-eddy simulation of the equatorial ocean boundary layer: Diurnal cycle, eddy viscosity and horizontal rotation. Journal of Geophysical Research, 101, 3649- 3662. doi:10.1029/95JC03441
[5] Wang, D., Large, W.G. and McWilliams, J.C. (1998) Large-eddy simulation of the diurnal cycle of deep equatorial turbulence. Journal of Physical Oceanography, 28, 129-148. doi:10.1175/1520-0485(1998)028<0129:LESOTD>2.0.CO;2
[6] Skyllingstad, E.D., Smyth, W.D., Moum J.N. and Wijesekera, H. (1999) Upper-ocean turbulence during a westerly wind burst: A comparison of large-eddy simulation results and microstructure measurements. Journal of Physical Oceanography, 29, 5-28. doi:10.1175/1520-0485(1999)029<0005:UOTDAW>2.0.CO;2
[7] Wang, D. and Müller, P. (2002) Effects of equatorial undercurrent shear on upper-ocean mixing and internal waves. Journal of Physical Oceanography, 32, 1041-1057. doi:10.1175/1520-0485(2002)032<1041:EOEUSO>2.0.CO;2
[8] Lien, R.-C, Caldwell, D.R., Gregg, M.C. and Moum, J.N. (1995) Turbulence variability at the equator in the central Pacific at the beginning of the 1991-1993 El Ni?o. Journal of Geophysical Research, 100, 6881-6898. doi:10.1029/94JC03312
[9] McPhaden, M.J. and Peters, H. (1992) Diurnal cycle of internal wave variability in the equatorial Pacific Ocean: Results from moored observations. Journal of Physical Oceanography, 22, 1317-1329. doi:10.1175/1520-0485(1992)022<1317:DCOIWV>2.0.CO;2
[10] Weingartner, T.J. and Weisberg, R.H. (1991) On the Annual Cycle of Equatorial Upwelling in the Central Atlantic Ocean. Journal of Physical Oceanography, 21, 68-82. doi:10.1175/1520-0485(1991)021<0068:OTACOE>2.0.CO;2
[11] Weingartner, T.J. and Weisberg, R.H. (1991) A descrip- tion of the annual cycle in sea surface temperature and upper ocean heat in the Equatorial Atlantic. Journal of Physical Oceanography, 21, 83-96. doi:10.1175/1520-0485(1991)021<0083:ADOTAC>2.0.CO;2
[12] Weisberg, T.J. and Tang, T.Y. (1987) Further studies on the response of the equatorial thermocline in the Atlantic Ocean to the seasonal varying trade winds. Journal of Geophysical Research, 92, 3709-3728. doi:10.1029/JC092iC04p03709
[13] Grodsky, S.A., Carton, J.A., Provost C., Servain, J., Lorenzetti, J.A. and McPhaden, M.J. (2005) Tropical instability waves at 0?N, 23?W in the Atlantic: A case study using PIRATA mooring data. Journal of Geo- physical Research, 110, C08010. doi:10.1029/2005JC002941
[14] Burchard, H., Bolding, K. and Villarreal, M. (1999) GOTM—a general ocean turbulence model. Theory, applications and test cases. European Commission Report EUR, European Commission.
[15] Burchard, H. and Bolding, K. (2001) Comparative analy- sis of four second-moment turbulence closure models for the oceanic mixed layer. Journal of Physical Oceano- graphy, 31, 1943-1968. doi:10.1175/1520-0485(2001)031<1943:CAOFSM>2.0.CO;2
[16] K. Bolding, k., Burchard, H., Pohlmann, T. and Stips, A. (2002) Turbulent mixing in the Northern North Sea: A numerical model study. Continental Shelf Research, 22, 2707-2724. doi:10.1016/S0278-4343(02)00122-X
[17] Jefrey, C.D., Robinson, I.S., Woolf, D.K. and Donlon C.J. (2008) The response to phase-dependent wind stress and cloud fraction of the diurnal cycle of SST and air–sea CO2 exchange. Ocean Modelling, 23, 33-48.
[18] Steiner, N. and Denman, K. (2008) Parameter sensitivities in a 1-D model for DMS and sulphur cycling in the upper ocean. Deep-Sea Research, 55, 847-865. doi:10.1016/j.dsr.2008.02.010
[19] Canuto, V.M., Howard, A., Cheng Y. and Dubovikov M.S. (2001) Ocean turbulence. Part I: One point closure model, momentum and heat vertical diffusivities. Journal of Physical Oceanography, 31, 1413-1426. doi:10.1175/1520-0485(2001)031<1413:OTPIOP>2.0.CO;2
[20] Fofonoff, N.P. and Millard, R.C. (1983) Algorithms for computation of fundamental properties of seawater. Unesco Technical Papers in Marine Science, 44, 53 pp.
[21] Servain, J., Busalacchi, A.J., McPhaden, M.J, Moura A.D., Reverdin, G., Vianna, M. and Zebiak, S.E. (1998) A pilot research moored array in the Tropical Atlantic (PIRATA). Bulletin of the American Meteorological Society, 79, 2019-2031. doi:10.1175/1520-0477(1998)079<2019:APRMAI>2.0.CO;2
[22] Bourlès, B., Lumpkin, R., McPhaden, M.J., Hernandez, F., Nobre, P., Campos, E., Yu, L., Planton, S., Busalacchi A., Moura, A.D., Servain, J. and Trotte, J., (2001) The PIRATA program: history, accomplishments, and future directions. Bulletin of the American Meteorological Society, 89, 1111-1125.
[23] Peres, J.R. (2008) Estudo do balan?o de radia??o sobre ooceano Atlantico Tropical na regi?o do Arquipélago de S?o Pedro e S?o Paulo (in portuguese), IAG. USP. 35 pp. http://www.iag.usp.br/meteo/labmicro/publicacoes/relatorios_tecnicos/Jean_2008-Estudo_do_balanco_de_radiacao_sobre_o_oceano_Atlantico_tropical_na_regiao_do_ASPSP.pdf
[24] Fairall, C.W., Bradley, E.F., Hare,J .E., Grachev, A.A. and Edson, J.B. (2003) Bulk parameterization of air-sea fluxes: updates and verification for the coare algorithm. Journal of Climate, 16, 571-591. doi:10.1175/1520-0442(2003)016<0571:BPOASF>2.0.CO;2
[25] Bolton, D. (1980) The computation of equivalent potential temperature. Monthly Weather Review, 108, 1046-1053. doi:10.1175/1520-0493(1980)108<1046:TCOEPT>2.0.CO;2
[26] Fairall, C.W., Bradley, E.F., Rogers, D.P., Edson, J.B. and Young G.S. (1996) Bulk parameterization of air-sea fluxes for the tropical ocean-global atmosphere coupled- ocean atmospheric response experiment. Journal of Geophysical Research, 101, 3747-3764. doi:10.1029/95JC03205
[27] Jerlov, N.G. (1968) Optical oceanography. American Elsevier Publ. Co., Inc., New York.
[28] Linden, P.F. (1975) The deepening of a mixed layer in a stratified fluid. The Journal of Fluid Mechanics, 71, 385- 405. doi:10.1017/S0022112075002637
[29] Philander, S.G. (1990) El Nino, La Nina and the Southern Oscillation. Academic Press, San Diego.

Copyright © 2024 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.