Nonlinear Parametrizations of Outgoing Longwave Radiation in Zero-Dimensional Energy Balance Models

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Authors

  • Dmitry V. Kovalevsky Saint Petersburg State University, Universitetskaya Emb. 7-9, 199034 St. Petersburg, Russia Author

DOI:

https://doi.org/10.5890/DNC.2016.09.004

Abstract

A one-layer and two-layer zero-dimensional (0D) energy balance models (EBMs) of the global climate system with different approximations for parametrization of outgoing longwave radiation (OLR) are considered. Three alternative approximations for parametrizing the OLR are explored in detail: (i) the (conventional) linear approximation, (ii) the quadratic approximation, and (iii) the ‘exact’ (power 4) model. In case of one-layer 0D EBM, exact analytical solutions are derived in closed form for all three alternative approximations for parametrizing the OLR. In the numerical examples provided, the deviations of the linear approximation from the ‘exact’ model are visible, while the quadratic approximation is virtually indistinguishable from the ‘exact’ model.

References

[1] Budyko, M. (1969), The effect of solar radiation variations on the climate of the Earth. Tellus, 21, 611-619.

[2] Sellers,W.D. (1969), A global climatic model based on the energy balance of the earth-atmosphere system, Journal of Applied Meteorology, 8, 392-400.

[3] Wu, W. and North, G.R. (2007), Thermal decay modes of a 2-D energy balance climate model, Tellus A, 59, 618-626.

[4] Rose, B.E.J. and Marshall, J. (2009), Ocean heat transport, sea ice, and multiple climate states: insights from energy balance models, Journal of the Atmospheric Sciences, 66, 2828-2843.

[5] Geoffroy, O., Saint-Martin, D., Olivié, D.J.L., Voldoire, A., Bellon, G. and Tytéca, S. (2013), Transient climate response in a two-layer energy-balance model. Part I: Analytical solution and parameter calibration using CMIP5 AOGCM experiments, Journal of Climate, 26, 1841-1857.

[6] IPCC (2013), Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.), Cambridge University Press: Cambridge, United Kingdom and New York, NY, USA.

[7] Pedlosky, J. (1987), Geophysical Fluid Dynamics, Second Edition, Springer-Verlag: New York.

[8] Dijkstra, H.A. (2005), Nonlinear Physical Oceanography: A Dynamical Systems Approach to the Large-Scale Ocean Circulation and El Ni?no, Second Edition, Kluwer Acad. Publishers: Dordrecht/Norwell, Mass.

[9] Ghil, M. (2016), A mathematical theory of climate sensitivity or, How to deal with both anthropogenic forcing and natural variability? In: Climate Change: Multidecadal and Beyond, World Scientific Series on Asia-Pacific Weather and Climate, Vol. 6, Chih-Pei Chang, M. Ghil, M. Latif and J.M. Wallace (eds.), World Scientific: New Jersey, 31-52.

[10] Lohmann, G. (2011), Abrupt climate change modelling, In: Extreme Environmental Events. Complexity in Forecasting and Early Warning, R.A. Meyers (ed.), Springer: New York, 1-21.

[11] Ciani, D., Carton, X., Bashmachnikov, I., Chapron, B. and Perrot, X. (2015), Influence of deep vortices on the ocean surface, Discontinuity, Nonlinearity, and Complexity, 4, 281-311.

[12] Mokhov, I.I. and Petoukhov, V.K. (1978), Parametrizacija uhodjashhej dlinnovolnovoj radiacii dlja klimaticheskih modelej [Parametrization of Outgoing Longwave Radiation for Climate Models], Moscow: IAP, USSR Academy of Sciences (preprint, in Russian).

[13] North, G.R., Cahalan, R.F. and Coakley, J.A. (1981), Energy balance climatemodels, Reviews of Geophysics and Space Physics, 19, 91-121.

[14] Alekseev, G.V. (1982), Vzaimodejstvie okeana i atmosfery kak termodinamicheskij process [Atmosphere-ocean interaction as a thermodynamic process], Transactions (Trudy) of AARI, 383, 25-34 (in Russian).

[15] Alekseev, G.V. and Podgorny, I.A. (1990), Simulation of advective global climate fluctuations, In: Research activities in atmospheric and oceanic modeling / C.J. Boer. GAS/JSC Working Group in Numerical Experimentation. 1990. Report 14. WMO/TD. 332. 7.24-7.25.

[16] Alekseev, G.V. and Podgorny, I.A. (1991), Advektivno-radiacionnye kolebanija klimata v sisteme atmosfera-okean- susha [Advective-radiative climate oscillations in the system atmosphere-ocean-land surface], Izvestiya of the USSR Academy of Sciences, Atmospheric and Oceanic Physics, 27, 1120-1129 (in Russian).

[17] Alekseev, G.V., Podgorny, I.A. and Svyashchennikov, P.N. (1990), Advektivno-radiacionnye kolebanija klimata [Advective-radiative climate oscillations], Transactions (Doklady) of the USSR Academy of Sciences, 315(4), 824-827 (in Russian).

[18] Alekseev, G.V. and Svyashchennikov, P.N. (1991), Estestvennaja izmenchivost' harakteristik klimata Severnoj poljarnoj oblasti i severnogo polusharija [Natural Variability of Climate Characteristics of the Northern Polar Region and the Northern Hemisphere], Gidrometeoizdat: Leningrad (in Russian).

[19] Kamke, E. (1959), Differentialgleichungen: Lösungsmethoden und Lösungen. I. Gewöhnliche Differentialgleichungen, 6. verbesserte Auflage, Leipzig.

[20] Dwight, H.B. (1961), Tables of Integrals and Other Mathematical Data, Fourth Edition, The Macmillan Company: New York.

[21] Hartmann, D.L. (1994), Global Physical Climatology, Academic Press: San Diego.

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How to Cite

Kovalevsky, D. V. (2026). Nonlinear Parametrizations of Outgoing Longwave Radiation in Zero-Dimensional Energy Balance Models. Discontinuity, Nonlinearity, and Complexity, 5(3), 239-249. https://doi.org/10.5890/DNC.2016.09.004