In 1997, reliable operation of the EISCAT Svalbard Radar (ESR) was achieved
and a rocket launching facility at Ny Alesund on Svalbard (79 degrees N, 1
2 degrees E) (SVALRAK) was established. On 20 November, 1977, the first ins
trumented payload was launched from SVALRAK. Although the payload configura
tion had been flown many times previously from Andoya Rocket Range on the N
orwegian mainland, this presented an unprecedented in situ determination of
positive ion density over Svalbard. Simultaneously, ESR measured similar d
ensity profiles but in a higher altitude regime. We have combined the ESR m
easurements with ionosonde data to establish a calibration and subsequently
combined the ground-based and in situ determined profiles to give a compos
ite positive ion density profile from the mesosphere to the thermosphere.