This paper presents the reduction results of ionosonde data and NNSS measured data at Manzhouli (38.07 mag. lat.) during 1983. The average behaviors and some anomalies of storm-time variations of the ionosphere above Manzhouli are obtained by analysing the critical frequency f
0F
2 and TEC N
T deduced from differential Doppler data.The results indicate that the behaviors of ionosphere in average show a typical seasonal anomaly and good agreement between the variations of f
0F
2 and N
T.Most of the ionospheric disturbances over Manzhouli is occurred in Equinox and Winter. The positive disturbances mostly happened in Winter, mixing positive and negative ones in Equinox, and negative ones in Summer and Equinox.It is shown that the good linear correlation is existed between the RMS value δ
Ap of magnetic index
Ap and the RMS deriations δN
T and δf
0F
2 from the month medians for TEC and f
0F
2 during magnetic storm.