European temperature variance from days to a decade is captured by a superposition of an AR(1) weather process, the yearly cycle, and an AR(2) mode with a 7-8 year oscillation in about half of the analyzed stations.
(C11) Here Fgi are the fluctuation functions of the AR(1) pro- cesses with parameters g1 and g2
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A simple decomposition of European temperature variability capturing the variance from days to a decade
European temperature variance from days to a decade is captured by a superposition of an AR(1) weather process, the yearly cycle, and an AR(2) mode with a 7-8 year oscillation in about half of the analyzed stations.