This study is conducted mainly by analyzing the characteristics of the scatter signal of the decameter-scale irregularities, which are mainly caused by temperature gradient instability and gradient drift instability (Thomas et al., 2014). Ionospheric irregularity refers to the ionization structure at various scales in the normal ionospheric structure, also known as ionospheric inhomogeneity. The size of the largest irregularity can be up to several thousand meters, and the smallest irregularity is only a few tens of centimeters. When the electromagnetic wave passes through the irregularities, its amplitude and phase change rapidly, which adversely affects navigation and communication.The Super Dual Auroral Radar Network (SuperDARN) was originally an international network of high-frequency (HF) coherent scattering radars that were built to observe the characteristics of ionospheric convection through the detection of decameter-scale, field-aligned, ionospheric irregularities in the polar region (Greenwald et al., 1995). With the observation data from SuperDARN radars, great signs of progress have been made in ionospheric convection (Chisham et al., 2007).However, the polar convection patterns during geomagnetic storms and substorms expand toward the equator, which gradually exceeded the observation range of the original radar network, which required the establishment of new radars in the mid-latitude region (Baker et al., 2007). The first mid-latitude SuperDARN radar was located at the grounds of the NASA Wallops Flight Facility (Baker et al., 2007), then, several mid-latitude radars were established continuously. Using the data from these mid-latitude HF radars, some studies have focused on phenomena in the mid-latitude ionosphere and proposed mechanisms to analyze them (Nishitani et al., 2019), such