In this paper computerized ionospheric tomographic technology has been appl
ied to investigate low-latitudinal ionospheric behavior during a moderate m
agnetic storm. From CT reconstructed imaging, during the main phase and rec
over phase both of positive and negative storm phases in low latitudinal io
nosphere are seen and they are not only latitude dependent but also height
dependent. It is certainly identified that a deep depletion in electron den
sity occurred just about 20 minutes after ssc at geomagnetic latitudes arou
nd 10 degrees where equatorial anomaly crest seats usually. The depleted ho
le extends over both the bottom and top F-region, with a steep wall on its
equatorial side. This is a very interesting low-latitude ionospheric respon
se to initial phase of storm and worthy of further study.