Sensitivity to initial conditions, the defining condition of a chaotic system, is an intrinsic property of the atmosphere. Ensemble spread is a proxy for the sensitivity of the atmosphere to its initial state. In this study, we calculate ensemble spread, relative to climatology, as well as its growth rate during each phase of the MJO. These calculations are performed globally to gain insight into the MJO's regional and global impacts on atmospheric predictability.
It will be shown that the MJO has statistically significant global impacts on predictability, even at locations that are well removed from the tropics. This is consistent with the view that the MJO has significant extratropical implications which can be either a response to, or a forcing for, the strong convection that often characterizes an MJO event. The strong relationship between the MJO and intrinsic predictability suggests that numerical weather models must struggle more during certain phases of the MJO in certain parts of the world.