In this paper, we study the geomagnetic storm that occurred on April 23–24, 2023. We present variations in the interplanetary magnetic field (IMF-Bz), solar wind parameters (Vsw, Nsw, Tsw, and Psw), geomagnetic index (SYM-H), and vertical total electron content (VTEC) derived from 18 GPS-TEC stations situated in equatorial, mid-latitude, and high-latitude regions. We analyze the Total Electron Content (TEC) variations before, during, and after the storm using VTEC plots, dTEC% plots, and global ionospheric maps for each GNSS receiver station, all referenced to Universal Time (UT). Our results indicate that GNSS receiver stations located at high latitudes exhibited an increase in ionospheric density structures during the main phase and a decrease during the recovery phase. In contrast, stations in equatorial and mid-latitude regions showed a decrease in ionospheric density during the main phase and an increase during the recovery phase. Large dTEC% values ranging from − 80 to 190 TECU were observed a few hours before and during the storm period (April 23–24, 2023), compared to values ranging from − 10 to 20 TECU on the day before (April 22, 2023) and the day after (April 25, 2023). Notably, higher dTEC% values were observed at stations in high and mid-latitudes compared to those in the equatorial region. As the storm progressed, the TEC intensification observed on global ionospheric maps appeared to shift from east to west. A detailed analysis of these maps showed that equatorial and low-latitude regions experienced the highest spatial and temporal TEC variations during the storm period compared to higher latitude regions.