During the NLC-93 rocket campaign at Esrange, Sweden, the vertical str
ucture of a noctilucent cloud layer has been investigated in situ. As
in earlier rocket flights, combinations of scattered light detectors a
nd electrostatic impact probes have been applied. While the photometri
c measurement provides the total downward radiance scattered from the
cloud particles, the impact probe yields local information about the p
article properties. The responses of both techniques scale differently
with the particle size. This feature is utilized to derive informatio
n about the height dependence of the particle population. The analysis
of three NLC passages indicates little vertical variation of the popu
lation throughout most of the layer. The lower part of the cloud is ch
aracterized by an increase in particle size and a decrease in particle
density towards the cloud base. This is to be expected for an NLC bri
ghtness peak caused by large particles sedimenting out of the cloud. I
mplications for the dynamical structure of the cloud are discussed.