[P-EM03] Mesosphere-Thermosphere-Ionosphere Coupling in the Earth's Atmosphere

[PEM03-P11] Fine structures in the E-region plasma density of the ionosphere observed by a Ca⁺ resonance scattering lidar observation

*江尻 省¹、西山 尚典¹、津田 卓雄²、阿保 真³、津野 克彦⁴、和田 智之⁴、小川 貴代⁴、川原 琢也⁵、中村 卓司¹ (1.国立極地研究所、2.電気通信大学、3.首都大学東京大学院システムデザイン研究科、4.理化学研究所、5.信州大学工学部)

キーワード：resonance scattering lidar, Ca+, fine structure, Sporadic E layer, interaction of neutral and plasma atmospheres

The National Institute of Polar Research (NIPR) is developing a new resonance scattering lidar with multiple wavelengths to install and operate it at Syowa, Antarctica. The lidar will observe temperature profiles and variations of minor constituents such as Fe, K, Ca⁺, and aurorally excited N₂⁺ in the mesosphere and lower thermosphere. In August 2014, it received the first light from Ca⁺ in a sporadic E layer. After that, we increase the resolution of the Ca+ observation and have succeeded in getting the Ca⁺ profile with time/height resolution of 5 sec/15 m. As a result of the high resolution observations, fine structures in a sporadic E layer with a vertical width of only 1 – 2 km have become detectable clearly. In this presentation, we will show the observed fine structures and discuss atmospheric instabilities in the E-region plasma.