Abstract
Climate is a special spatiotemporal dynamical system. Its time scale can be extended indefinitely, but its space scale can never exceed that of the size of the system. We call this a “mismatching” in space and time domains. With the help of a simplified system of primitive equations, this exploratory paper shows that these scale characteristics may have a significant impact on the mathematical and physical structure of the system. The results show that the mismatching of space–time scales will lead to a decrease of the system’s dimension, degenerating the system from an infinite dimensional to a finite one. Also they show that “mismatched” domains can lead to a greater consistency of the system’s structure in space, as they form a system of uniform structures which are described as “patches”. This may lead to an alternative way of representing climate and its variability as a pattern system defined by the collective behavior of interacting patches or subsystems.
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References
Duan MK, Zhou XJ (2014) Stochastic dynamic simulation of the 100-kyr cycles in climate system. Sci China Earth Sci 58(3):420–428
Fountalis I, Bracco A, Dovrolis C (2013) Spatio-temporal network analysis for studying climate patterns. Clim Dyn. https://doi.org/10.1007/s00382-013-1729-5
Fujita T (1963) Analytical mesometeorology: a review, severe local storms. Meteoral Monogr 27:77–128. https://doi.org/10.1007/978-1-940033-56-3-5
Held IM (2005) The gap between simulation and understanding in climate modeling. Bull Am Meteoral Soc. https://doi.org/10.1175/BAMS-86-11-1609
Latif M (2011) Uncertainty in climate change projections. J Geochem Explor 110:1–7
Luan YH, Yu YQ, Zheng WP (2016) Review of development and application of high resolution global climate system model. Adv Earth Sci 31(3):258–268. https://doi.org/10.11867/j.issn.1001-8166.2016.03.0258
Majda AJ, Christian Franzke C, Crommelin D (2009) Normal forms for reduced stochastic climate models. Proc Natl Acad Sci 106(10):3649–3653. https://doi.org/10.1073/pnas.0900173106
North GR, Coakley JA (1979) Differences between seasonal and mean annual energy balance model calculations of climate and climate sensitivity. J Atmos Sci. https://doi.org/10.1175/1520-0469(1979)0362.0.CO;2
Orlanski I (1975) A rational subdivision of scales for atmospheric processes. Bull Am Meteorol Soc. https://doi.org/10.1155/2013/525383
Philips NA (1956) The general circulation of the atmosphere: a numerical experiment. Q J R Meteorol 352(82):123–164. https://doi.org/10.1002/qj.49708235202
Saltzman B (2001) Dynamical paleoclimatology: generalized theory of global climate change. Academic Press, 354
Steinhaeuser K, Tsonis AA (2013) A climate model intercomparison at the dynamics level. Clim Dyn. https://doi.org/10.1007/s00382-013-1761-5
Tsonis AA, Wang G, Swanson K, Rodrigues FA, da Fontura Costa L (2010) Community structure and dynamics in climate networks. Clim Dyn 37:933–940. https://doi.org/10.1007/s00382-010-0874-3
Acknowledgements
This research was partially supported by the National Key R&D Program of China (2017YFC1501804) and the National Natural Science Foundation of China (42075054, 91737102 and 41575058). Useful discussions with Dr. Tianjun Zhou and Dr. Cheng-Zhi Zou are gratefully acknowledged. The authors are grateful to the three anonymous referees and Dr. Tamas Bodai for their useful comments that helped to improve the quality of the manuscript.
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Yang, P., Wang, G., Xiao, Z. et al. Climate: a dynamical system with mismatched space and time domains. Clim Dyn 56, 3305–3311 (2021). https://doi.org/10.1007/s00382-021-05646-7
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DOI: https://doi.org/10.1007/s00382-021-05646-7