“…One of the main equipment on monitoring scintillations is the ionospheric scintillation monitoring receiver (ISMR), which can provide two types of indices: the amplitude scintillation index (
) and the phase scintillation index (
). Due to the differences in the generation mechanism of ionospheric scintillation in the low latitude and the polar regions (Luan et al.,
2015; Mitchell et al.,
2005), amplitude scintillations often occur in the low latitude region, while phase scintillations dominate in the polar region (Zhao, Li, Wang, et al.,
2022). To reflect the variation information of the scintillation in the Arctic region, which is the interest area of this research, the phase scintillation index will be extensively studied in this paper.…”