The Taylor hypothesis, which allows surrogating spatial measurements requir
ing many experimental probes : by rime series from one or two probes, is ex
amined on the basis of a simple analytic model of turbulent statistics. The
main points are as follows: (i) The Taylor hypothesis introduces systemati
c errors in the evaluation of scaling exponents. (ii) When the mean wind (V
) over bar(0) is not infinitely larger than the root-mean-square longitudin
al turbulent fluctuations upsilon(T), the effective Taylor advection veloci
ty V-ad Should take the latter into account. (iii) When two or more probes
are employed the application of the Taylor hypothesis and the optimal choic
e of the effective advecting wind V-ad need extra care. We present practica
l considerations for minimizing the errors incurred in experiments using on
e or two probes. (iv) Analysis of the Taylor hypothesis when different prob
es experience different mean winds is offered. [S1063-651X(99)14010-8].