NASA sounding rocket 21.114, launched March 7, 1998, during the Coqui II ca
mpaign, provided neutral wind and plasma density measurements of a weak int
ermediate layer. The layer was centered near 140 km and had an approximate
peak plasma density of 2200 cm(-3). The measured winds were typically less
than 40 m s(-1), in agreement with wind shear formation theory and coincide
nt density observations. The data obtained during the flight allow us to ex
plore the plasma density structure and wind field morphology of the interme
diate layer. Coupled with simultaneous data from Arecibo Observatory, the u
pleg and downleg density profiles provide three spatially separated measure
ments that enable the first detailed investigation of the horizontal extent
and variation of an intermediate layer.