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We construct a network from climate records of atmospheric temperature atsurface level, at different geographical sites in the globe, using reanalysisdata from years 1948-2010. We find that the network correlates with the NorthAtlantic Oscillation (NAO), both locally in the north Atlantic, and throughcoupling to the southern Pacific Ocean. The existence of tele-connection linksbetween those areas and their stability over time allows us to suggest apossible physical explanation for this phenomenon.

Global Climate network evolves with North Atlantic Oscillation phases: Coupling to Southern Pacific Ocean