Optical observations of 557.7 nm and 630.0 nm emissions from discrete
auroral arcs in the post-noon sector have been related to localised fi
eld-aligned enhancements in the spatial distribution of E- and F-layer
electron density respectively seen in images reconstructed by ionosph
eric tomography. Results from two case studies are presented in which
meridian scanning photometer and all-sky camera observations on Svalba
rd have been compared to electron-density structures found by tomograp
hic inversion of measurements made by reception of radio signals at a
chain of four stations at high latitude. The F-layer features are long
-lived and show exact correspondence to the red-line emissions. Transi
ent arcs in green-line intensity result in E-region structures that ar
e resolved in one case, but not in another where the dynamic auroral f
orms are separated by less than one degree of latitude. The signature
of an inverted-V precipitation event is clearly evident in one example
.