“…The strength of EIA asymmetry is calculated by taking the ratio of the maximum value of the two hemispheric anomaly TEC crests values. Besides the meridional neutral winds, dragging force due to continuous ion accumulation, sudden stratospheric warming, solar fluxes, atmospheric tides, change in composition due to magnetic perturbations, and photochemical process are also responsible factors for the asymmetry of the EIA peaks (Abdu et al, , ; Dang et al, ; Goncharenko et al, ; Hanson & Moffett, ; Immel et al, ; Jonah et al, ; Khadka et al, ; Tulasi Ram et al, ; Xiong et al, ). In this study, we particularly focused on analyzing the contribution of meridional neutral wind for the asymmetry generation of EIA using observational and modeled winds in the low‐latitude ionosphere.…”