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11 - Teleconnections and Patterns of Variability

from Flows of Energy

Published online by Cambridge University Press:  25 February 2022

Kevin E. Trenberth
Affiliation:
National Center for Atmospheric Research
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Summary

The weather systems undergo incredibly rich variety and never repeat. If left alone in the atmosphere, mid-latitude storms would continually march eastwards, modulated by very large-scale atmospheric waves – planetary waves – set up by the land–sea differences and continental mountain ranges. The latter are mainly in evidence in the northern hemisphere and vary from summer to winter because the mid- to high-latitude land is colder than the adjacent seas in winter, but warmer in summer. Nevertheless, this idealized state seldom exists and frequently the weather systems get stuck into a certain repeating pattern of sorts, called weather regimes.

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Publisher: Cambridge University Press
Print publication year: 2022

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References

References and Further Reading

Hurrell, J. W., Kushnir, Y., Ottersen, G., and Visbeck, M., 2003: An overview of the North Atlantic Oscillation. In: Hurrell, J. W., Kushnir, Y., Ottersen, G., and Visbeck, M., eds. The North Atlantic Oscillation: Climatic Significance and Environmental Impact. Geophysical Monograph 134, 135. Washington, DC: American Geophysical Union.Google Scholar
Kwok, R., and Comiso, J. C., 2002: Spatial patterns of variability in Antarctic surface temperature: connections to the Southern Hemisphere Annular Mode and the Southern Oscillation. Geophysical Research Letters, 29, 1705, doi: 10.1029/2002GL015415.CrossRefGoogle Scholar
Marshall, G. J., 2003: Trends in the Southern Annular Mode from observations and reanalyses. Journal of Climate, 16, 41344143. doi: 10.1175/1520-0442(2003)016<4134:TITSAM>2.0.CO;2.Google Scholar
Trenberth, K. E., 1990: Recent observed interdecadal climate changes in the Northern Hemisphere. Bulletin of the American Meteorological Society, 71, 988993.2.0.CO;2>CrossRefGoogle Scholar
Trenberth, K. E., 2015: Has there been a hiatus? Science, 349(2649), 691692. doi: 10.1126/science.aac9225.CrossRefGoogle ScholarPubMed
Trenberth, K. E., and Hurrell, J. W., 1994: Decadal atmosphere–ocean variations in the Pacific. Climate Dynamics, 9, 303319.CrossRefGoogle Scholar
Trenberth, K. E., and Hurrell, J. W., 2019: Climate change. In: Dunn, P. O., and Møller, A. P., eds., The Effects of Climate Change on Birds, 2nd ed. Oxford: Oxford University Press, 5–25.Google Scholar
Trenberth, K. E., and Shea, D. J., 2006: Atlantic hurricanes and natural variability in 2005. Geophysical Research Letters, 33, L12704. doi: 10.1029/2006GL026894.CrossRefGoogle Scholar
Trenberth, K. E., Branstator, G. W., Karoly, D., Kumar, A., Lau, N-C., and Ropelewski, C., 1998: Progress during TOGA in understanding and modeling global teleconnections associated with tropical sea surface temperatures. Journal of Geophysical Research, 103 , 1429114324.Google Scholar
Trenberth, K. E., Jones, P. D., Ambenje, P., et al., 2007: Observations: surface and atmospheric climate change. In: Solomon, S., Qin, D., Manning, M., et al., eds., Climate Change 2007. The Physical Science Basis. Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press, 235336.Google Scholar

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