Ground observations have been used to study the ionosphere by providing ele
ctron density profiles and TEC distribution, In this paper, the existing gr
ound and space facilities related to constructing the Constellation Observi
ng System for Meteorology, ionosphere, and Climate (COSMIC) Project are rev
iewed. We show that these observations can be employed to validate results
derived from COSMIC satellites. In addition, the NCAR TIEGCM model is intro
duced to simulate ionosphere TEC during year of the solar minimum. The obse
rvations and simulations present a clear signature of the equatorial anomal
y, in which the TEC shows a minimum on the magnetic equator and a maximum o
n each side. Meanwhile, it is interesting to see that the value of TEC in J
une (Day 170) becomes weaker with the crests moving toward the geomagnetic
equator.