We present a new approach to model the Ionosphere based on GPS data. P
revious authors have used models with an unique shell. In this case we
have included a second shell to account for the distribution of the e
lectrons in the outer part of the Ionosphere. We have analyzed the ion
ospheric electron content of a region above 30 degrees in declination
in different conditions of ionospheric activity using the Kalman filte
r. The data used has been obtained from the International GPS Service
fop Geodynamics (IGS) network. Simultaneously we have studied the rece
iver and transmitter differential biases showing the effects of neglec
ting the outer part of the Ionosphere in the model. It appears a syste
matic variations for the receivers-depending on its latitude-not for t
he satellites.