A coupled ocean-atmosphere model of relevance to the ITCZ in the eastern Pacific

References

• Anderson, D. L. T. and McCreary, J. P. 1985. Slowly propagating disturbances in a coupled ocean-atmosphere model. J. Atmos. Sci. 42, 615–929.
   Web of Science ®Google Scholar
• Charney, J. G. 1969. The intertropical convergence zone and the Hadley circulation of the atmosphere. Proc. WMOIIUGG Symposium on Numerical weather prediction in Tokyo, III-73-111-79, Japan Meteor. Agency.
   Google Scholar
• Esbensen, S. K. and Kushnir, V. 1981. The heat budget of the global Ocean: An atlas based on estimates from surface marine observations. Report 29, 27 pp., 188 figs., Clim. Res. Inst., Oreg. State Univ., Corvallis.
   Google Scholar
• Gill, A. E. 1980. Some simple solutions for heat-induced tropical circulation. Quart. J. Roy. Meteor. Soc. 106, 447–462.
   Web of Science ®Google Scholar
• Graham, N. E. and Barnett, T. P. 1987. Sea surface temperature, surface wind divergence and convection over tropical oceans. Science 238, 657–659.
   Web of Science ®Google Scholar
• Hansen, J. E. et al. 1988. Global climate changes as forecasted by Goddard Institute for Space Studies three-dimension model. J. Geophys. Res. 93, 9341–9364.
   Web of Science ®Google Scholar
• Hayashi, Y. Y. and Sumi, A. 1986. The 30-40 day oscillations simulated in an “Aqua Planet” model. J. Meteor. Soc. Japan 64, 451–467.
   Web of Science ®Google Scholar
• Herbert, D., Mourn, J. N. and Caldwell, D. R. 1991. Does ocean turbulence peak at the equator, revisited. J. Phys. Oceanogr. 21, 1690–1698.
   Web of Science ®Google Scholar
• Hess, P. G., Battisti, D. S. and Rasch, P. J. 1993. The maintenance of the intertropical convergence zones and the large-scale tropical circulation on a water-covered earth. J. Atmos. Sci. 50, 691–713.
   Web of Science ®Google Scholar
• Hubert, L. F., Krueger, A. F. and Winston, J. S. 1969. The double intertropical convergence zone-Fact or fiction? J. Atmos. Sci. 26, 771–773.
   Web of Science ®Google Scholar
• Kornfield, J., Hasler, A. F., Hanson, K. J. and Suomi, V. E. 1967. Photographic cloud climatology from ESSA III and V computer produced mosaics. Bulletin Amer. Meteor. Soc. 48, 878–882.
   Web of Science ®Google Scholar
• Kraus, E. B. and Turner, J. S. 1967. A one-dimensional model of the seasonal thermocline. (II). The general theory and its consequences. Tellus 19, 98–109.
   Google Scholar
• Levitus, S. 1982. Climatological atlas of the world ocean. NOAA professional paper no. 13, 173 pp. U.S. Government Printing Office, Wahington, DC.
   Google Scholar
• Manabe, S., Hahn, D. G. and Holloway, J. L.Jr. 1974. The seasonal variation of the tropical circulation as simulated by a global model of the atmosphere. J. Amos. Sci. 31, 43–83.
   Google Scholar
• Manabe, S., Bryan, K. and Spelman, M. J. 1975. A global ocean-atmosphere climate model. Part I. The atmospheric circulation. J. Phys. Oceanogr. 5, 3–29.
   Web of Science ®Google Scholar
• Matsuno, T. 1966. Quasi-geostrophic motions in the equatorial area. J. Meteor. Soc. Japan 44, 25-43. Mitchell, T. P. and Wallace, J. M. 1992. The annual cycle in equatorial convection and sea surface temperature. J. Climate 5, 1140–1156.
   Google Scholar
• Mourn, J. N. and Galdwell, D. R. 1985. Local influences on shear-flow turbulence in the equatorial ocean. Science 230, 315–316.
   Web of Science ®Google Scholar
• Niiler, P. P. and Kraus, E. B. 1977. One-dimensional models of the upper ocean. Modeling and prediction of the upper layers of the ocean, E. B. Kraus, Ed. Pergamon, 143-172.
   Google Scholar
• Numaguti, A. and Hayashi, Y.-Y. 1991. Behaviors of the cumulus activity and the structures of the circulations in the “aqua-planet” model. Part II: Large-scale structures and evaporation-wind feedback. J. Meteor. Soc. Japan 69, 563–579.
   Google Scholar
• Oberhuber, J. M. 1988. An Atlas based on the “COADS” data set: The budgets of heat, buoyancy and turbulent kinetic energy at the surface of the global ocean. Report no. 15, 20 pp. + figs. Max-Planck-Institut fur Meteor., Hamburg.
   Google Scholar
• Philander, S. G. H. and Seigel, A. D. 1985. Simulation of El Nitio of 1982-1983. Coupled ocean-atmosphere models, J. C. J. Nihoul, ed. Elsevier Oceanogr. Series, 40, Elsevier, 517-541.
   Google Scholar
• Pike, A. C. 1971. Intertropical convergence zone studied with an interacting atmosphere and ocean model. Mon. Wea. Rev. 99, 469–477.
   Web of Science ®Google Scholar
• Rasmusson, E. M. and Carpenter, T. H., 1982. Variations in tropical sea surface temperature and surface wind fields associated with the Southern Oscillation/ El Niño. Mon. Wea. Rev. 110, 354–384.
   Web of Science ®Google Scholar
• Reed, R. K. 1977. On estimating insolation over the ocean. J. Phys. Oceanogr. 7,482–485.
   Web of Science ®Google Scholar
• Schopf, P. S. and Cane, M. A. 1983. On equatorial dynamics, mixed layer physics and sea surface temperature. J. Phys. Oceanogr. 13,917–935.
   Web of Science ®Google Scholar
• Wang, B. and Li, T. 1992. A simple tropical atmosphere model of relevance to short-term climate variations. Part I: Model physics. J. Atmos. Sci. 50, 260–284.
   Web of Science ®Google Scholar
• Weare, B. C., Strub, P. T. and Samuel, M. D. 1981. Annual mean surface heat fluxes in the tropical Pacific Ocean./. Phys. Oceanogr. 11, 705–717.
   Web of Science ®Google Scholar
• Wright, P. B. 1988. An Atlas based on the “COADS” data set: fields of mean wind, cloudiness and humidity at the surface of the global ocean. Report no. 14, 7 pp. + figs., Max-Planck-InstitutfurMeteor., Hamburg.
   Google Scholar
• Xie, S.-P., 1994. On the genesis of the equatorial annual cycle. J. Climate, in press.
   Google Scholar
• Xie, S.-P., Kubokawa, A. and Hanawa, K. 1989. Oscillations with two feedback processes in a coupled ocean-atmosphere model. J. Climate 2, 946–964.
   Web of Science ®Google Scholar