The outdoor experiments, using a metallic grid above the ground surfac
e, have yielded well-defined vertical profiles of the space-charge den
sity. The profiles showed strong evidence for the existence of an elec
trode effect, which could be named the artificial electrode effect and
can serve as a very useful and well-controlled model for the study of
atmospheric electric processes in the atmospheric surface layer. The
build-up or break-down of an electrode-effect layer occurred in a time
of the order of 10 s under the experimental conditions realized. The
artificially generated electrode effect is dependent on the electrical
field strength supplied, wind speed, turbulent mixing and ion mobilit
ies. Wind speed and ion mobility seem to be the dominant factors, defi
ning space-charge density profiles. A theoretical model for the artifi
cial electrode effect has been developed, taking into account turbulen
t mixing of charged particles in the air flow with the logarithmic pro
file of the wind velocity. The numerical analysis of the boundary valu
e problem for the two-dimensional equations for the light ion concentr
ations has been performed. The model presented shows a qualitative agr
eement of calculated space-charge profiles with measured ones, and exp
lains the dependence of the artificial electrode effect on the dominan
t control parameters. The limiting conditions for the developed theory
are discussed.