Insights into atmospheric predictability through global convection-permitting model simulations

This potential, however, depends on the predictability of the atmosphere, which was explored here through identical twin experiments using the Model for Prediction Across Scales. The simulations were produced on a quasi-uniform 4-km mesh, which allowed the illumination of error growth from convective to global scales.

During the first two days, errors grew through moist convection and other mesoscale processes, and the character of the error growth resembled the case of k(-5/3) turbulence. Between 2 and 13 days, errors grew with the background baroclinic instability, and the character of the error growth mirrored the case of k(-3) turbulence. The existence of an error growth regime with properties similar to k(-5/3) turbulence confirmed the radical idea of E. N. Lorenz that the atmosphere has a finite limit of predictability, no matter how small the initial error.