Day-to-day variations in the growth of uncertainty in the current state of
the atmosphere have led to operational ensemble weather predictions in whic
h an ensemble of different initial conditions, each perturbed from the best
estimate of the current state and yet still consistent with the observatio
ns, is forecast. Contrasting competing methods for the selection of ensembl
e members is a subject of active research; the assumption that the ensemble
members represent sufficiently small perturbations so as to evolve within
the "linear regime'' is implicit to several of these methods. This regime,
in which the model dynamics are well represented by a linear approximation,
is commonly held to extend to 2 or 3 days for operational forecasts. It is
shown that this is rarely the case. A new measure, the relative nonlineari
ty, which quantifies the duration of the linear regime by monitoring the ev
olution of "twin'' pairs of ensemble members, is introduced. Both European
and American ensemble prediction systems are examined; in the cases conside
red for each system (87 and 25, respectively), the duration of the linear r
egime is often less than a day and never extends to 2 days. The internal co
nsistency of operational ensemble formation schemes is discussed in light o
f these results. By decreasing the optimization time, a modified singular v
ector-based formation scheme is shown to improve consistency while maintain
ing traditional skill and spread scores in the seven cases considered. The
relevance of the linear regime to issues regarding data assimilation, adapt
ive observations, and model sensitivity is also noted.