To understand the water level fluctuation characteristics at the groundwater observation network installed and operated in the area around Seoraksan National Park, a time series analysis of long-term data of groundwater levels observed in the network from 2012 to 2021 was performed. The observation network comprises three locations, all installed in the bedrock aquifer, and periodic inspections and management are carried out by the relevant operating agency. According to the linear analysis results, the groundwater level decreased by -89.7 cm/yr at the Goseong-Inheung Observatory, whereas it rose by 3.7 cm/yr at the Goseong-Toseong Observatory. A strong autocorrelation was observed among the three observatories. In particular, at the Goseong-Inheung Observatory, the time delay was found to be approximately 8 times longer than that at the Goseong- Toseong and Sokcho-Nohak observatories, whereas the time delay of precipitation was similar to the time delay of Goseong-Toseong and Sokcho-Nohak. These results were judged to have strong linearity and memory effects with the groundwater level data. Analysis of the cross-correlation function between rainfall and groundwater levels showed that Goseong-Inheung had a certain degree of cross-correlation with rainfall, with a delay of 12 days. If the discharge in major rivers of Seoraksan National Park is continuously monitored, researches on water resources using river discharge and groundwater levels are expected to be actively conducted.
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