Abstract
A coupled general circulation model has been used to perform a set of experiments with high CO2 concentration (2, 4, 16 times the present day mean value). The experiments have been analyzed to study the response of the climate system to strong radiative forcing in terms of the processes involved in the adjustment at the ocean–atmosphere interface. The analysis of the experiments revealed a non-linear response of the mean state of the atmosphere and ocean to the increase in the carbon dioxide concentration. In the 16 × CO2 experiment the equilibrium at the ocean–atmosphere interface is characterized by an atmosphere with a shut off of the convective precipitation in the tropical Pacific sector, associated with air warmer than the ocean below. A cloud feedback mechanism is found to be involved in the increased stability of the troposphere. In this more stable condition the mean total precipitation is mainly due to large-scale moisture flux even in the tropics. In the equatorial Pacific Ocean the zonal temperature gradient of both surface and sub-surface waters is significantly smaller in the 16 × CO2 experiment than in the control experiment. The thermocline slope and the zonal wind stress decrease as well. When the CO2 concentration increases by about two and four times with respect to the control experiment there is an intensification of El Niño. On the other hand, in the experiment with 16 times the present-day value of CO2, the Tropical Pacific variability weakens, suggesting the possibility of the establishment of permanent warm conditions that look like the peak of El Niño.













Similar content being viewed by others
References
An S-I, Wang B (2000) Interdecadal change of the structure of the ENSO mode and its impact on the ENSO frequency. J Clim 13:2044–2055
Blanke B, Delecluse P (1993) Low frequency variability of the tropical Atlantic ocean simulated by a General Circulation Model with mixed-layer physics. J Phys Oceanogr 23:1363–1388
Boccaletti G, Pakanowski RC, Philander SGH (2004) The thermal structure of the upper ocean. J Phys Oceanogr 34:888–902
Boer GJ, Hamilton K, Zhu W (2005) Climate sensitivity and climate change under strong forcing. Clim Dyn 24:685–700
Capotondi A, Wittenberg A, Masina S (2006) Spatial and temporal structure of Tropical Pacific interannual variability in 20th century coupled simulations. Ocean Model 15:274–298
Clement AC, Seager R, Cane MA, Zebiak SE (1996) An ocean dynamical thermostat. J Clim 9:2190–2196
Collins M (2000) The El Niño Southern Oscillation in the second Hadley Center coupled model and its response to greenhouse warming. J Clim 13:1299–1312
Da Silva A, Young AC, Levitus S (1994) Atlas of Surface Marine Data 1994, vol 1: algorithms and procedures. NOAA Atlas NESDIS 6, U.S. Department of Commerce, Washington, D.C
Fedorov AV, Dekens PS, McCarthy M, Ravelo AC, deMenocal PB, Barreiro M, Pacanowski RC, Philander SGH (2006) The Pliocene Paradox (Mechanisms for a permanent El Niño). Science 312:1485–1489
Fichefet T, Morales Maqueda MA (1999) Modelling the influence of snow accumulation and snow-ice formation on the seasonal cycle of the Antarctic sea-ice cover. Clim Dyn 15:251–268
Gualdi S, Navarra A, Guilyardi E, Delecluse P (2003) Assessment of the tropical Indo-Pacific climate in the SINTEX CGCM. Ann Geophys 46:1–26
Gualdi S, Scoccimarro E, Navarra A (2008) Changes in tropical cyclone activity due to global warming: results from a high-resolution coupled general circulation model. J Clim (in press)
Guilyardi E (2006) El Ni no-mean state-seasonal cycle interactions in a multi-model ensemble. Clim Dyn 26:329–348
Guilyardi E, Delecluse P, Gualdi S, Navarra A (2003) Mechanisms for ENSO phase change in a coupled GCM. J Clim 16:1141–1158
Held IM, Soden BJ (2006) Robust responses of the hydrological cycle to global warming. J Clim 19:5686–5699
Houghton JT, Meira Filho LG, Callender BA, Harris N, Kattenberg A, Maskell K (eds) (1995) Climate change 1995: the science of climate change. Contribution of Working Group I to the second assessment of the Intergovernmental Panel on Climate Change. Cambridge University Press, UK, 572 pp
Houghton JT, Ding Y, Griggs DJ, Noguer M, van der Linden PJ, Xiaosu D (eds) (2001) Climate change 2001: the scientific basis. Contribution of Working Group I to the third assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge, 881 pp
Huang RX, Pedlosky J (2000) Climate variability of the equatorial thermocline inferred from a two-moving-layer model of the ventilated thermocline. J Phys Oceanogr 30:2610–2626
Knutson TR, Manabe S (1995) Time-mean response over the tropical Pacific to increased CO2 in a coupled ocean–atmosphere model. J Clim 8:2181–2199
Liu Z, Vavrus S, He F, Wen N, Zhong Y (2005) Rethinking tropical ocean response to global warming: the enhanced equatorial warming. J Clim 18:4684–4700
Madec G, Delecluse P, Imbard M, Levy C (1998) OPA version 8.1 Ocean general circulation model reference manual. Tech Rep LODYC/IPSL Note 11
Manabe S, Wetherald RT (1967) Thermal equilibrium of the atmosphere with a given distribution of relative humidity. J Atmos Sci 24:241–259
Masina S, Di Pietro P, Navarra A (2004) Interannual-to-decadal variability of the North Atlantic from an ocean data assimilation system. Clim Dyn 23:531–546
McPhaden MJ, Zhang D (2002) Slowdown of the meridional overturning circulation in the upper Pacific Ocean. Nature 415:603–608
Mechoso CR, Robertson AW, Barth N, Davey MK, Delecluse P, Gent PR, Ineson S, Kirtman B, Latif M, LeTreut H, Nagal T, Neelin JD, Philander SGH, Polcher J, Schopf PS, Stockdale T, Suarez MJ, Terray L, Thual O, Tribbia JJ (1995) The seasonal cycle over the tropical Pacific in coupled ocean–atmosphere general circulation models. Mon Weather Rev 123:2825–2838
Meehl GA, Gent P, Arblaster JM, Otto-Bliesner B, Brady E, Craig A (2001) Factors that affect amplitude of El Niño in global coupled climate models. Clim Dyn 17:515–526
Meehl GA, Teng H, Branstator G (2006) Future changes of El Niño in two global coupled models. Clim Dyn 26(6):549–566
Merryfield WJ (2006) Changes to ENSO under CO2 doubling in a multi-model ensemble. J Clim 19:4009–4027
Pierrehumbert RT (1995) Thermostats, radiator fins and the local runaway greenhouse. J Atmos Sci 52(10):1784–1806
Ramanathan V, Collins W (1991) Thermodynamic regulation of ocean warming by cirrus clouds deduced from observations of the 1987 El Niño. Nature 351:27–32
Ramanathan V, Collins W (1992) Thermostat and global warming. Nature 357:649
Rayner NA, Parker DE, Horton EB, Folland CK, Alexander LV, Rowell DP, Kent EC, Kaplan A (2003) Global analysis of sea surface temperature, sea ice and night marine air temperature since the late nineteenth century. J Geophys Res 18(D14):4407. doi:10.1029/2002JD002670
Roeckner E, Arpe K, Bengtsson L, Christoph M, Claussen M, Dümenil L, Esch M, Giorgetta M, Schlese U, Schulzweida U (1996) The Atmospheric general circulation Model ECHAM4: model description and simulation of present-day climate. Max-Planck Institut für Meteorologie, Report no. 218, Hamburg, 86 pp
Soden BJ, Held IM (2006) An assessment of climate feedbacks in coupled ocean–atmosphere models. J Clim 19:3354–3360
Soden BJ, Jackson DL, Ramaswamy V, Schwarzkopf MD, Huang X (2005) The radiative signature of upper tropospheric warming. Science 310:841–844
Timmermann A, Oberhuber J, Bacher A, Esch M, Latif M, Roeckner E (1999) Increased El Niño frequency in a climate model forced by future greenhouse warming. Nature 398:694–696
Trenberth KE, Smith L (2006) The vertical structure of temperature in the tropics: different flavours of El Niño. J Clim 19:4956–4970
Trenberth KE, Jones PD, Ambenje P, Bojariu R, Easterling D, Klein Tank A, Parker D, Rahimzadeh F, Renwick JA, Rusticucci M, Soden BJ, Zhai P (2007) Observations: surface and atmospheric climate change. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Climate Change 2007: the physical science basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge
Valcke S, Terray L, Piacentini A (2000) The Oasis coupler user guide version 2.4. Tech Rep TR/CMGC/00-10, CERFACS
Vecchi GA, Soden BJ (2007) Global warming and the weakening of the tropical circulation. J Clim 20:4316–4340
Vecchi GA, Soden BJ, Wittenberg AT, Held IM, Leetma A, Harrison MJ (2006) Weakening of tropical Pacific atmospheric circulation due to anthropogenic forcing. Nature 441:73–76
Wallace JM (1992) Effect of deep convection on the regulation of tropical sea surface temperature. Nature 357:230–231
Zhang GJ, McPhaden MJ (1995) The relationship between sea surface temperature and latent heat flux in the Equatorial Pacific. J Clim 8:589–605
Acknowledgments
We thank the European Community project DYNAMITE, contract 003903-GOCE, for the financial support. We are grateful to S. Gualdi, E. Scoccimarro and all the INGV people involved in the coupling of the SINTEXG model. Particularly, we thank the two anonymous reviewers whose suggestions and constructive criticism have significantly improved the manuscript.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Cherchi, A., Masina, S. & Navarra, A. Impact of extreme CO2 levels on tropical climate: a CGCM study. Clim Dyn 31, 743–758 (2008). https://doi.org/10.1007/s00382-008-0414-6
Received:
Accepted:
Published:
Issue date:
DOI: https://doi.org/10.1007/s00382-008-0414-6


