“…Furthermore, to reduce the impact of multipath, the 20‐degree elevation mask is adopted, which was utilized by previous scintillation investigations (e.g., Béniguel, 2019; Salles et al., 2021; Veettil et al., 2020). Meanwhile, to avoid other nonscintillation‐related disturbances on BDS signals, 0.2 is selected as the threshold of the amplitude scintillation index S 4 indicating the occurrence of ionospheric scintillation at the given epoch (Luo et al., 2020; Muella et al., 2009, 2014; Pasumarthi et al., 2020; Zhao et al., 2022), characterized by the standard deviation of I /< I >, where I is the received signal intensity (power) and < > represents temporal averaging, typically during a 60‐s interval, assuming a sampling frequency of 50 Hz (Luo et al., 2020; Moraes et al., 2019; Song et al., 2022; Sousasantos et al., 2018), to indicate the occurrence of ionospheric scintillation. Ionospheric scintillation events were further classified as weak (0.2 ≤ S 4 < 0.4), moderate (0.4 ≤ S 4 < 0.6), and intense ( S 4 ≥ 0.6) (Humphreys et al., 2010; Vilà‐Valls et al., 2020).…”