Hydrological cycle and ocean stratification in a coupled climate system: a theoretical study

References

• Bryan, F. 1986. High-latitude salinity effects and interhemispheric thermohaline circulation. Nature 323, 301–304.
   Web of Science ®Google Scholar
• Craig, G. C. 1996. Dimensional analysis of a convecting atmosphere in equilibrium with external forcing. Q. J. R. MeteoroL Soc. 122, 1963–1967.
   Web of Science ®Google Scholar
• Dessler, A. E. and Sherwood, S. C. 2000. Simulations of tropical upper tropospheric humidity. J. Geophys. Res. 105,20155–20163.
   Web of Science ®Google Scholar
• Emanuel, K. A. 1994. Atmospheric Convection. Oxford University Press, York, 580 pp.
   Google Scholar
• Emanuel, K. A. and Bister, M. 1996. Moist convective velocity and buoyancy scales. J. Atmos. Sci. 53 (22), 3276–3285.
   Web of Science ®Google Scholar
• Emanuel, K. A., Neelin, J. D. and Bretherton, C. S. 1994. On large-scale circulations in convecting atmospheres. Q. J. R. MeteoroL Soc. 120, 1111–1143.
   Web of Science ®Google Scholar
• Follcins, I., Kelly, K. K. and Weinstock, E. M. 2002. A simple explanation for the increase in relative humidity between 11 and 14 km in the tropics. J. Geophys. Res. 107 (D23), 4736, 10.1029/2002JD002185
   Web of Science ®Google Scholar
• Hartmann, D. L. and Michelsen, M. L. 1993. Large-scale effects on the regulation of tropical sea surface temperature. J. Climate 6, 2049–2062.
   Web of Science ®Google Scholar
• Held, I. M., Hemler, R. S. and Ramaswamy, V. 1993. Radiative-convective equilibrium with explicit two-dimensional moist convection. J. Atmos. Sc i. 50, 3909–3927.
   Google Scholar
• Held, I. M. and Soden, B. J. 2000. Water vapor feedback and global warming. Annu. Rev. Energy Environ. 25,441–475.
   Google Scholar
• Held, I. M. and Soden, B. J. 2006. Robust responses of the hydrological cycle to global warming. J. Climate 19, 5686–5699.
   Web of Science ®Google Scholar
• Huang, R. X. 1994. Thermohaline circulation: energetics and variability in a single-hemisphere basin model. J. Geophys. Res. 99, 12,471-12,485.
   Google Scholar
• Huang, R. X. 1999. Mixing and energetics of the oceanic thermohaline circulation. J. Phys. Oceanogr 29, 727–746.
   Web of Science ®Google Scholar
• Kleidon, A., Fraedrich, K., Kunz, T. and Lunkeit, F. 2003. The atmospheric circulation and states of maximum entropy production. Geophys. Res. Lett. 30 (23), 2223, 10.1029/2003GL018363.
   Web of Science ®Google Scholar
• Kleidon, A., and Lorenz, R. D. 2005. Non-equilibrium Thermodynamics and the Production of Entropy: Life, Earth, and Beyond. Springer, Heidelberg, 260 pp.
   Google Scholar
• Knutson, T. R. and Manabe, S. 1995. Time-mean response over the tropical Pacific to increased CO2 in a coupled ocean-atmosphere model. J. Climate 8, 2181–2199.
   Web of Science ®Google Scholar
• Lorenz, E. N. 1967. The Nature and Theory of the General Circulation of the Atmosphere. World Meteorological Organization, Geneva, 161 pp.
   Google Scholar
• Lorenz, R. D. and McKay, C. P. 2003. A simple expression for vertical convective fluxes in planetary atmospheres. Icarus 165, 407–413.
   Web of Science ®Google Scholar
• Manabe, S. and Strickler, R. F. 1964. Thermal equilibrium of the atmosphere with a convective adjustment. J. Atmos. Sc i. 21, 361–385.
   Web of Science ®Google Scholar
• Manabe, S. and Stouffer, R. J. 1994. Multiple-century response of a coupled ocean-atmosphere model to an increase of atmospheric carbon dioxide. J. Climate 7, 5–23.
   Web of Science ®Google Scholar
• Manabe, S. and Wetherald, R. T. 1967. Thermal equilibrium of the atmosphere with a given distribution of relative humidity. J. Atmos. Sc i. 24, 241–259.
   Web of Science ®Google Scholar
• Mitas, C. M. and Clement, A. 2005. Has the Hadley cell been strengthening in recent decades? Geophys. Res. Lett. 32, L03809, 10.1029/2004GL021765.
   Web of Science ®Google Scholar
• Neumann, G. and Pierson, W. J. Jr. 1966. Principles of Physical Oceanography. Prentice-Hall, Englewood Cliffs, NJ, 545 pp.
   Google Scholar
• Ou, H. W. 2001. Possible bounds on the earth’s surface temperature: from the perspective of a conceptual global-mean model. J. Climate 14, 2976–2988.
   Web of Science ®Google Scholar
• Ou, H. W. 2006. Thermal properties of a coupled ocean-atmosphere: a conceptual model. Tellus 58 (3), 404–415.
   Google Scholar
• Ozawa, H., Ohmura, A., Lorenz, R. D. and Pujol, T. 2003. The second law of thermodynamics and the global climate system: a review of the maximum entropy production principle. Rev. Geophys. 41,4/10182003.
   Web of Science ®Google Scholar
• Pauluis, O. and Held, I. M. 2002. Entropy budget of an atmosphere in radiative-convective equilibrium. Part I: maximum work and frictional dissipation. J. Atmos. Sci. 59 (2), 125–139.
   Web of Science ®Google Scholar
• Peixoto, J. P. and Oort, A. H. 1992. Physics of Climate. American Institute of Physics, New York, 520 pp.
   Google Scholar
• Pierrehumbert, R. T. 1995. Thermostats, radiator fins, and the local runaway greenhouse. J. Atmos. Sc i. 52, 1784–1806.
   Google Scholar
• Pierrehumbert, R. T. 1998. Lateral mixing as a source of subtropical water vapor. Geophys. Res. Lett. 25 (2), 151–154.
   Web of Science ®Google Scholar
• Pierrehumbert, R. T. 1999. Subtropical water vapor as a mediator of rapid global climate change. In: Mechanisms of Global Change at Millennial Time Scales (eds P. U. Clark, R. S. Webb, and L. D. Keigwin). American Geophysical Union, Washington, DC, Geophysical Monograph Series 112,394 pp.
   Google Scholar
• Pierrehumbert, R. T. and Roca, R. 1998. Evidence for control of Atlantic Subtropical humidity by large scale advection. Geophys. Res. Lett. 25, 4537–4540.
   Web of Science ®Google Scholar
• Rahmstorf, S. 1995. Bifurcations of the Atlantic thermohaline circulation in response to changes in the hydrological cycle. Nature 378, 145–149.
   Web of Science ®Google Scholar
• Renno, N. O. 1997. Multiple equilibria in radiative-convective atmospheres. Tellus 49A, 423–438.
   Google Scholar
• Renno, N. O. and Ingersoll, A. P. 1996. Natural convection as a heat engine: a theory for CAPE. J. Atmos. Sc i. 53, 572–585.
   Web of Science ®Google Scholar
• Robe, E R. and Emanuel, K. A. 1996. Moist convective scaling: some inferences from three-dimensional cloud ensemble simulations. J. Atmos. Sci. 53 (22), 3265–3275.
   Web of Science ®Google Scholar
• Schmittner, A. and Stocker, T. F. 1999. The stability of the thermohaline circulation in global warming experiments. J. Climate 12, 1117–1133.
   Web of Science ®Google Scholar
• Shimokawa, S. and Ozawa, H. 2002. On the thermodynamics of the oceanic general circulation: irreversible transition to a state with higher rate of entropy production. Q. J. R. Meteorol. Soc. 128,2115–2128.
   Web of Science ®Google Scholar
• Shine, K. P. and Sinha, A. 1991. Sensitivity of the earth’s climate to height-dependent changes in the water vapor mixing ratio. Nature 354, 382–384.
   Web of Science ®Google Scholar
• Spencer, R. W. and Braswell, W. D. 1997. How dry is the tropical free troposphere? Implications for global warming theory. Bull. Am. Met. Soc. 78, 1097–1106.
   Web of Science ®Google Scholar
• Stephens, G. L. 1990. On the relationship between water vapor over the oceans and sea surface temperature. J. Climate. 3, 634–645.
   Web of Science ®Google Scholar
• Stephens, G. L. and Webster, P. J. 1979. Sensitivity of radiative forcing to variable cloud and moisture. J. Atmos. Sci. 26, 1542-1556.
   Google Scholar
• Stommel, H. and Csanady, G. 1980. A relation between the T-S curve and global heat and atmospheric water transports. J. Geophys. Res. 85, 495–501.
   Web of Science ®Google Scholar
• Sui, C. H., Lau, K. M., Tau, W. K. and Simpson, J. 1994. The tropical water and energy cycles in a cumulus ensemble model. Part I: equilibrium climate.J. Atmos. Sci. 51 (5), 711-728.
   Google Scholar
• Sun, D.-Z. and Lindzen, R. L. 1993. Distribution of tropical tropospheric water vapor. J. Atmos. Sci. 50 (12), 1643–1660.
   Web of Science ®Google Scholar
• Sun, D. and Oort, A. H. 1995. Humidity-temperature relationships in the tropical troposphere. J. Climate 8, 1974–1987.
   Web of Science ®Google Scholar
• Tippins, D. and Tomczak, M. 2003. Meridional turner angles and density compensation in the upper ocean. Ocean Dyn. 53, 332–342.
   Google Scholar
• Trenberth, K. and Caron, J. 2001. Estimates of meridional atmosphere and ocean heat transports. J. Climate 14, 3433-3443.
   Web of Science ®Google Scholar
• Turner, J. R. 1979. Buoyancy Effects in Fluids. Cambridge University Press, Cambridge, 368 pp.
   Google Scholar
• Veronis, G. 1973. Model of the world ocean circulation: I. Wind-driven, two-layer. J. Mar Res. 31, 228–288.
   Web of Science ®Google Scholar
• Weaver, A. J., Marotzke, J., Cummins, P. E and Sarachilc, E. S. 1993. Stability and variability of the thermohaline circulation.J. Phys. Oceanogr 23, 39-60.
   Google Scholar
• Webster, P. J. 1994. The role of hydrological processes in ocean-atmosphere interactions.Rev. Geophys. 32, 427-476.
   Google Scholar
• Wunsch, C. 1998. The work done by the wind on the oceanic general circulation. J. Phys. Oceanogr 28, 2332–2340.
   Web of Science ®Google Scholar
• Wunsch, C. 2002. What is the thermohaline circulation? Science 298, 1179–1180.
   PubMed Web of Science ®Google Scholar