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A simple conceptual model to interpret the 100 000 years dynamics of paleo-climate records

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Fig. 1. Panel (a):(in years) associated with the labeled frequencies are: (1) 1789;(2) 1079; (3) 860; (4) 667; (5) 566; (6) 438; (7) 322; (8) 295;its frequency spectra
Fig. 2.Fig. 2. Panel (a): Maximal oscillation amplitude A = max(x(t))min(x(t)) as a function of the forcing amplitude F in absence ofnoise
Table 1. Main periods obtained from the single ensemble of thesimulation with and (first column)
Table 2. Labels (first column), main periods obtained from theGISP2 δ18O record (second column), autocorrelation maxima forthe solar forcing (F.A.M, third column) and main periods obtainedfrom the simulations, for time interval I (early ice age) (top) andti

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