Tomographic images are presented from a co-ordinated experimental camp
aign held in Scandinavia in October 1993. In addition to the five sate
llite receiving stations, the EISCAT incoherent scatter radar was used
in a special mode (SP-UK-BLOB) to provide independent verification of
the tomographic images. The radar was used in this interactive made t
o follow the meridional development of a very steep field-aligned grad
ient at the poleward edge of a deep trough. Irregular structuring on a
scale of tens of kilometres was observed as the feature was followed
during a 7-hour run, under very quiet geomagnetic conditions. Several
satellite passes were monitored during the run, with the total electro
n content measurements being used to reconstruct tomographic images of
electron density. Comparison of the images with the EISCAT measuremen
ts in the vicinity of the trough wall shows that the field-aligned str
ucture is well replicated by the tomographic method. The auroral E-lay
er evident in the EISCAT observations has also been imaged by tomograp
hic means for the first time.