The tomographic reconstruction technique generates a two-dimensional l
atitude versus height electron density distribution from sets of slant
total electron content measurements (TEC) along ray paths between bea
con satellites and ground-based radio receivers. In this note, the tec
hnique is applied to TEC values obtained from data simulated by the Sh
effield/UCL/SEL Coupled Thermosphere/Ionosphere/Model (CTIM). A compar
ison of the resulting reconstructed image with the 'input' modelled da
ta allows for verification of the reconstruction technique. All the fe
atures of the high-latitude ionosphere in the model data are reproduce
d well in the tomographic image. Reconstructed vertical TEC values fol
low closely the modelled values, with the F-layer maximum density (NmF
2) agreeing generally within about 10%. The method has also been able
successfully to reproduce underlying auroral-E ionisation over a restr
icted latitudinal range in part of the image. The height of the F2 pea
k is generally in agreement to within about the vertical image resolut
ion (25 km).