Separate a smooth large-scale velocity from a remaining smaller-scale component . If the large-scale variation length is much greater than , their longitudinal increment has the form
For a positive integer , the leading expansion of its structure function is
Thus even a velocity component at scales much larger than enters through its gradients and through mixed moments with the finer field. It is not generally legitimate to discard those mixed moments: large-scale strain can organize and modulate the finer motions. For example, at fourth order the expansion contains
in addition to the small-scale fourth moment and the generally present odd mixed terms. Even if the components were independent and symmetric, the displayed mixed second-moment term would survive. This explicitly exhibits large-scale contributions to structure functions beyond second order.
The implication for K62 refined similarity is that an observed structure function need not measure a purely scale-local velocity fluctuation. Dividing it by may still leave dependence on outer-scale gradients, correlations or finite-range cutoffs. The universal conditional coefficients and the identification of a measured exponent with the lognormal intermittency model therefore require additional locality and scale-separation tests. Finite-range mixed contributions can imitate or obscure anomalous scaling. This is an objection to treating the 1962 dimensional argument as an unconditional law for measured increments; it is not, by itself, a proof that an asymptotic refined similarity regime cannot exist.