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War 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2. A composite temperature spectrum: the GRIP (Summit) ice core δ 18 O a temperature proxy, low resolution (left, brown) along with the first 91 kyr at high resolution (left, green), ◦ with the spectrum of the (mean) 75 N 20th Century reanalysis temperature spectrum, at 6 h resolution, from 1871–2008, at 700 mb (right). The overlap (from 10–138 yr scales) is used for calibrating the former (moving them vertically on the log-log plot). All spectra are averaged over logarithmically spaced bins, ten per order of magnitude in frequency. Three regimes are shown corresponding to the weather regime with βw = 2 (the diurnal variation and subharmonic at 12 h are visible at the extreme right). The central macro weather “plateau” is shown along with the theoretically predicted βmw = 0.2–0.4 regime. Finally, at longer time scales (the left), a new scaling climate regime with exponent βc ≈ 1.4 continues to about 100 kyr. Reproduced from Lovejoy and Schertzer (2012d). 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