An intrinsic pink-noise multi-decadal global climate dynamics mode

Understanding multi-decadal variability is an essential aspect of climate dynamics. For example, the recent phenomenon referred to as the "global warming hiatus" may reflect a coupling to an intrinsic, pre-industrial, multi-decadal variability process. Here, using a multi-fractal time series method, we demonstrate that forty-two data sets of seventy-nine proxies with global coverage exhibit the same pink ($\sim$ $1/f$) noise characteristics on multi-decadal time scales. To quantify the persistence of this behavior, we examine high-resolution ice core and speleothem data to find pink noise in both pre- and post-industrial periods. We examine the spatial structure with Empirical Orthogonal Function (EOF) analysis of the monthly-averaged surface temperature from 1901 to 2012. The first mode clearly shows the distribution of ocean heat flux sinks located in the eastern Pacific and the Southern Ocean and has pink noise characteristics on a multi-decadal time-scale. We hypothesize that the combination of this pink noise multi-decadal spatial mode may resonate with externally-driven greenhouse gas forcing leading to substantial changes in the global temperature.