Vertical fine structure and time evolution of plasma irregularities in the E s layer observed by a high-resolution Ca + lidar

The vertical fine structures and the time evolution of plasma irregularities in the sporadic E (Es) layer were observed via calcium ion (Ca+) density measurements using a resonance scattering lidar with a high time-height resolution (5 s and 15 m) at Tachikawa (35.7°N, 139.4°E) on December 24, 2014. The observation successfully provided clearer fine structures of plasma irregularities, such as quasi-sinusoidal height variation, localized clumps, “cats-eye” structures, and twist structures, in the sporadic Ca+ (\({{\text{Ca}}^{+}}_{\text{s}}\)) layers at around 100 km altitude. These fine structures suggested that the Kelvin–Helmholtz instabilities occurred in the neutral atmosphere whose density changed temporarily or spatially. The maximum Ca+ density in the \({{\text{Ca}}^{+}}_{\text{s}}\) layer was two orders of magnitude smaller than the maximum electron density estimated from the critical frequency (foEs) simultaneously observed by the ionosonde at Kokubunji (35.7°N, 139.5°E). A strong positive correlation with a coefficient of 0.91 suggests that Ca+ contributes forming the Es layer as well as major metallic ions Fe+ and Mg+ in the lower thermosphere. Moreover, the formation of a new \({{\text{Ca}}^{+}}_{\text{s}}\) layer at 110 km and the upward motions of the \({{\text{Ca}}^{+}}_{\text{s}}\) layers at 100 km and 110 km were observed before the local sunrise and just after the sunrise time at the conjugation point. Although the presence or absence of a causal relationship with the sunrise time was not clear, a possible explanation for the formation and the upward motions of the \({{\text{Ca}}^{+}}_{\text{s}}\) layers was the occurrence of strong horizontal wind, rather than the enhancement of the eastward electric field. Open image in new window