Skip to main content
Log in

A comparison of vertical mixing schemes embedded in an OGCM with application to air-sea interactions and the evolution of SST anomalies

  • Published:
Meteorology and Atmospheric Physics Aims and scope Submit manuscript

Summary

The performance of three different vertical mixing schemes embedded in a global coarse resolution OGCM under both annual and monthly mean forcing are compared. These schemes are the integral model of Kraus and Turner and the differential parametrisations of Pacanowski and Philander and Henderson-Sellers (EDD1 scheme). The simulations of mean climatological conditions suggest that, with respect to climate change studies, the Kraus-Turner and the EDD1 schemes are overall more robust than the Pacanowski and Philander parametrisation. With respect to anomalous climatic conditions (i.e. decay of imposed SST anomalies), all three schemes indicate that the lifespan and penetration depth of a cold anomaly is somewhat greater than for a warm one. Also, the EDD1 scheme portrays the evolution process of the SST anomalies somewhat differently than the other two schemes.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Adamec, D., Elsberry, R. L., Garwood, R. W., Jr., Haney, R. L., 1981: An embedded mixed layer-ocean circulation model.Dyn. Atmos. Oceans,5, 69–96.

    Google Scholar 

  • Alderson, S. G., 1990: On embedding a mixed layer model into an ocean general circulation model.Dyn. Atmos. Oceans,15, 59–86.

    Google Scholar 

  • Bryan, K., 1969: A numerical method for the study of the circulation of the world ocean.J. Computat. Phys.,4, 347–376.

    Google Scholar 

  • Bryan, K., Lewis, L. J., 1979: A water mass model of the world ocean.J. Geophys. Res.,84, 2503–2517.

    Google Scholar 

  • Cox, M. D., 1984: A primitive equation, 3-dimensional model of the ocean.GFDLOcean Group Technical Report No. 1, Princeton University.

  • Esbensen, S. K., Kushnir, Y., 1981: The heat budget of the global ocean: an atlas based on estimates from surface marine observations.Oregon State University Climate Research Institute Report,29, 27 pp.

  • Foreman, S. J., 1986: Ocean and atmosphere interact.Meteor. Mazine. 115, 358–361.

    Google Scholar 

  • Gaspar, Ph., 1988: Modelling the seasonal cycle of the upper ocean.J. Phys. Oceanogr.,18, 161–180.

    Google Scholar 

  • Gaspar, Ph., Gregoris, Y., Stull, R., Boissier, Ch., 1988: Long-term simulations of upper ocean vertical mixing using models of various types. In: Nihoul, J. C. J., Jamart, B. M. (eds.)Small-Scale Turbulence and Mixing in the Ocean. 19th International Liege Colloquim on Ocean Hydrodynamics, Elsevier, 169–184.

  • Hellerman, S., Rosenstein, M., 1983: Normal monthly wind-stress over the world ocean with error estimates.J. Phys. Oceanogr.,13, 1093–1104.

    Google Scholar 

  • Henderson-Sellers, B., 1985: New formulation of eddy diffusion thermocline models.Appl. Math. Medel.,9, 441–446.

    Google Scholar 

  • Henderson-Sellers, B., 1988: Embedding stratification models in ocean general circulation climate models. In: Nihoul, J. C. J., Jamart, B. M. (eds.)Small-Scale Turbulence and Mixing in the Ocean. 19th International Liege Colloquim on Ocean Hydrohynamics. Elsevier, 95–107.

  • Kraus, E. B., 1988: Merits and defects of different approaches to mixed layer modelling In: Nihoul, J. C. J., Jamart, B. M. (eds.)Small-Scale Turbulence and Mixing in the Ocean. 19th International Liege Colloquim on Ocean Hydrodynamics. Elsevier, 37–50.

  • Kraus, E. B., Turner, J. S., 1967: A one-dimensional model of the seasonal thermocline. II: The general theory and its consequences.Tellus,19, 98–105.

    Google Scholar 

  • Kraus, E. B., Bleck, R., Hanson, H. P., 1988: The inclusion of a surface mixed-layer in a large-scale circulation model. In: Nihoul, J. C. J., Jamart, B. M. (eds.)Small-Scale Turbulence and Mixing in the Ocean. 19th International Liege Colloquim on Ocean Hydrodynamics. Elsevier, 51–62.

  • Kühnel, I., Henderson-Sellers, B., 1991: Mixed layer modelling with respect to ocean-atmosphere interactions in the eastern Indian Ocean.Meterol. Atmos. Phys. 46, 51–64.

    Google Scholar 

  • Levitus, S., 1982: Climatological atlas of the world ocean. NOAA Professional Paper,13, U.S. Govt. Printing Office, 173 pp.

  • Mellor, G. L., Yamada, T., 1982: Development of a turbulence closure model for geophysical fluid problems.Rev. Geophys. Space Phys.,20, 851–857.

    Google Scholar 

  • Moore, A. M., Reason, C. J. C., 1993: The response of a global ocean general circulation model to climatological surface boundary conditions for temperature and salinity.J. Phys. Oceanogr. (in press).

  • Niiler, P. P., Kraus, E. B., 1977: One-dimensional models of the upper oceans. In: Kraus, E. B. (eds.)Modelling and Prediction of the Upper Layers of the Ocean. Pergamon, 143–172.

  • Pacanowski, R. C., Philander, S. G. H., 1981: Parameterization of vertical mixing in numerical models of tropical oceans.J. Phys. Oceanogr.,11, 1443–1451.

    Google Scholar 

  • Philander, S. G. H., 1990:El Nino, La Nina, and the Southern Oscillation. San Diego: Academic Press, 289 pp.

    Google Scholar 

  • Reason, C. J. C., 1993: On the effect of ENSO precipitation anomalies in a global OGCM.Clim. Dyn. (in press).

  • Rosati, A., Miyakoda, K., 1988: A general circulation model for upper ocean simulation.J. Phys. Oceanogr.,18, 1601–1626.

    Google Scholar 

  • Semtner, A. J. Jr., Chervin, R. M., 1988: A simulation of the global ocean circulation with resolved eddies.J. Geophys. Res. 93, 15, 502–515, 222.

    Google Scholar 

  • Smith, T. N., Gordon, H. B., 1992: Simulations of precipitation and atmospheric circulation changes associated with warm SSTs: results from an ensemble of long term integrations with idealized anomalies.Climate Dyn.,7, 141–153.

    Google Scholar 

  • Verron, J., Le Provost, C., 1991: Response of eddy-resolved general circulation numerical models to asymmetrical wind forcing.Dyn. Atmos. Oceans. 15, 505–533.

    Google Scholar 

  • Wacongne, S., 1988.The Dynamics of the Equatorial Undercurrent and its Termination. PhD thesis, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Additional information

With 9 Figures

Rights and permissions

Reprints and permissions

About this article

Cite this article

Reason, C.J.C., Kühnel, I. & Henderson-Sellers, B. A comparison of vertical mixing schemes embedded in an OGCM with application to air-sea interactions and the evolution of SST anomalies. Meteorl. Atmos. Phys. 51, 55–71 (1993). https://doi.org/10.1007/BF01080880

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF01080880

Keywords

Navigation