Timeālapse seismic data processing is an important technique for observing subsurface changes over time. The conventional timeālapse seismic exploration has been conducted using a largeāscale exploration system. However, for efficient monitoring of shallow subsurface, timeālapse monitoring based on the smallāscale exploration system is required. Smallāscale exploration system using a sparker source offers high vertical resolution and cost efficiency, but it faces challenges, such as inconsistent waveforms of sparker sources, inaccurate positioning information and a low signalātoānoise ratio. Therefore, this study proposes a data processing workflow to preserve the signal and enhance the repeatability of smallāscale timeālapse seismic data acquired using a sparker source. The proposed workflow has three stages: preāstack, postāstack and machine learningābased data processing. Conventional seismic data processing methods were applied to enhance the quality of the sparker seismic data during the preāstack data processing stage. In the postāstack processing stage, the positions and energy correction were performed, and the machine learningābased data processing stage attenuated random noise and applied a matched filter. The data processing was performed using only the seismic signals recorded near the seafloor, and the results confirmed the improvement in the repeatability of the entire seismic profile, including that of the target area. According to the repeatability quantification results, the predictability increased and the normalized root mean square decreased during data processing, indicating improved repeatability. In particular, the repeatability of the data was greatly improved through vertical correction, energy correction and matched filtering approaches. The processing results demonstrate that the data processing method proposed in this study can effectively enhance the repeatability of highāresolution timeālapse seismic data. Consequently, this approach could contribute to a more accurate understanding of temporal changes in subsurface structure and material properties.