Abstract
Research activities at all stages of analysis constitute preliminary steps for the most important task—time series forecasting. One of such stages includes efforts to understand statistical properties of the processes that are being studied including probability density functions, spectral densities, and the degree of statistical predictability. Climate is often regarded as a Markov process with a small parameter, which means a slowly and monotonically decreasing spectral density without any oscillations and/or quasi-periodic phenomena. Many climatic time series and indices including AO and AAO, NAO, PDO, AMO, and PNA behave in agreement with that Markov model or even with white noise. The climate indices related to ENSO behave in a different manner: their spectra are nonmonotonic and contain a smooth maximum at about 0.2 cpy. Yet, none of them contains regular oscillations and their predictability stays low. The annual surface temperature for 1920–2018 averaged over large parts of the globe generally does not follow the Markov model, and its predictability is relatively high. Some other oscillatory processes are studied as well, including a version of AAO and MJO—a bivariate random process whose scalar components are shown to possess some statistical predictability.
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Appendix
Appendix
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Privalsky, V. (2021). Stochastic Models and Spectra of Climatic and Related Time Series. In: Time Series Analysis in Climatology and Related Sciences. Progress in Geophysics. Springer, Cham. https://doi.org/10.1007/978-3-030-58055-1_5
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