The Global Positioning System (GPS) observables are affected by the io
nosphere. The dispersive nature of this effect and the use of two freq
uencies in the GPS observations make possible to measure the ionospher
ic total electron content (TEC) from dual frequency GPS data. In this
work we test the concept of permanent monitoring of TEC using a networ
k of GPS receivers at high latitudes. We have used GPS data from five
permanent receivers in Scandinavia, from 1-30 January 1994, with geogr
aphic latitudes ranging from 57.4 degrees N to 78.9 degrees N. The res
ults show the capability of the method to monitor the evolution of TEC
as a function of time and geographical location. We have detected nig
ht-time enhancements almost every night for some of the stations, and
we have also been able to produce maps of the instantaneous TEC as a f
unction of both latitude and longitude around the GPS network. We also
present some of the current limitations in the use of GPS for estimat
ing TEC at high latitudes such as the difficulties in solving for cycl
e-slips, and the necessity of reliable values for the receiver and sat
ellite differential instrumental biases.