Hamiltonian distributed chaos in large-scale climate dynamics

It is shown that the large-scale climate dynamics, represented by the daily indices of the North Atlantic (NAO), Pacific/North American (PNA), Arctic (AO) and Antarctic (AAO) oscillations, Asian-Australian Monsoons (ISM, WNPM and AUSM) and El Nino/La Nina phenomenon (Nino indices) as well as the global temperature anomalies (land), is dominated by the Hamiltonian distributed chaos with the stretched exponential spectrum.