Comparison of the Heights of Sporadic E Layers and Vertical Ion Convergence Parameters

Abstract

Sporadic E (Es) layers are thin layers of enhanced electron density that commonly appear at altitudes of 90–130 km, often impacting radio communications and navigation systems. The wind shear theory posits that the vertical ion drift, influenced by atmospheric neutral winds and the magnetic field, serves as a significant dynamic driver for the formation and movement of Es layers. In current studies, both the heights of ion vertical velocity null (IVN) and the maximum vertical ion convergence (VICmax) have been proposed as the potential height of Es layer occurrence. In this study, utilizing the neutral atmospheric wind data derived from the WACCM-X (The Whole Atmosphere Community Climate Model with thermosphere and ionosphere extension), we computed and compared these two parameters with the observed Es layer heights recorded by the FORMOSAT-3/COSMIC (FORMOsa SATellite-3/Constellation Observing System for Meteorology, Ionosphere, and Climate) radio occultation (RO) observations. The comparative analysis suggests that IVN is a more likely node for Es layer occurrence than VICmax. Subsequently, we examined the height–time distributions of IVN and Es layers, as well as their respective descent rates at different latitudes. These results demonstrated a notable agreement in height variations between IVN and Es layers. The collective results presented in this paper provide strong support that the ion vertical velocity null plays a crucial role in determining the height of Es layers.

Enhanced Sporadic E Layer and Its Perturbations During the 2022 Hunga Volcanic Eruption

“…Mid-latitude Es layer is a prominent phenomenon in the atmosphere-ionosphere coupling system because its formation process is generally controlled by the interaction between neutral wind shears and metallic ions acting in the presence of the Earth's magnetic field (Haldoupis, 2011;Whitehead, 1989). Observations and simulations have confirmed that the Es layer occurrence has significant diurnal and semidiurnal behaviors associated with atmospheric tides (Andoh et al, 2022;Moro et al, 2023;Qiu et al, 2023b;Sobhkhiz-Miandehi et al, 2022;Yamazaki et al, 2021;Yu et al, 2023).…”