Climate Predictions: The Chaos and Complexity in Climate Models

Figure 6

Kolmogorov complexity for the (a) precipitation and (b) air temperature time series for Belgrade and (c) precipitation and (d) temperature for Novi Sad, in Serbia, obtained from climate simulations using different models. On 𝑥-axis are depicted the values of the time series normalized as 𝑥_𝑖=(𝑋_𝑖−𝑋_min)/(𝑋_max−𝑋_min), where {𝑋_𝑖} is the time series of the precipitation or air temperature, 𝑋_max=max{𝑋_𝑖}, and 𝑋_min=min{𝑋_𝑖}.

(a)

(b)

(c)

(d)