Japan Geoscience Union Meeting 2025

Presentation information

[E] Poster

P (Space and Planetary Sciences ) » P-EM Solar-Terrestrial Sciences, Space Electromagnetism & Space Environment

[P-EM14] Study of coupling processes in solar-terrestrial system

Wed. May 28, 2025 5:15 PM - 7:15 PM Poster Hall (Exhibition Hall 7&8, Makuhari Messe)

convener:Mamoru Yamamoto(Research Institute for Sustainable Humanosphere, Kyoto University), Yasunobu Ogawa(National Institute of Polar Research), Satonori Nozawa(Institute for Space-Earth Environmental Research, Nagoya University), Akimasa Yoshikawa(Department of Earth and Planetary Sciences, Kyushu University)

5:15 PM - 7:15 PM

[PEM14-P03] Resonance-scattering Ca/Ca+ lidar precisely observing the upper atmosphere: simultaneous observation of Ca and Ca+ layers and measurement of Ca+ temperature

*Masayuki Katsuragawa1,2, Mutsumi K Ejiri2,3, Ayaka Hashimoto1, Sota Kobayashi1, Sayako Miyoshi1, Hikaru Miyagi1, Ken'ichi Nakagawa1, Takuo T Tsuda1, Chiaki Ohae1, Takuji Nakamura2,3 (1.University of Electro-Communications, 2.National institute of Polar Research, 3.The Grad. Univ. for Advanced Studies)

Keywords:Resonance Scattering Lidar, Ca, Ca+ ion, Ti:sapphire laser

To observe the upper atmosphere from the ground with a high temporal and spatial resolution, we have developed a resonant-scattering Ca/Ca+ lidar that can simultaneously observe both meteoric Ca and Ca+. The system is based on a solid-state laser (the dual-wavelength injection-locked nanosecond pulsed Ti:sapphire laser), providing a major benefit of operating stably for long periods. As the development of this lidar system has reached a practically applicable stage and a preliminary operation has been also tested, the simultaneous observation of Ca and Ca+ over a long time has been attempted. We could successfully conduct the simultaneous observation of Ca and Ca+ for an entire night (December 24, 2024). We found that the complex spatio-temporal behaviors of Ca and Ca+ were very similar to each other although their detailed density-distributions were different. We also observed a relatively dense Ca+ layer a few kilometers deep that appeared at the uppermost altitude in the observed range of 80 – 105 km, being recognized as a formation of a sporadic E layer.

The developed resonant-scattering Ca/Ca+ lidar has a high frequency-purity and a high frequency-accuracy, thereby, giving it the ability to also measure temperature and wind/drift of the target atoms/ions in the observed altitude range by measuring the Doppler broadened resonance profile. In fact, we conducted a preliminary test of Ca+ temperature observation continuously for one hour. In the presentation, in addition to the details of the Ca+ temperature measurements, we will also discuss what new insights we have gained from this new lidar, including comparisons with data from the ionosonde observation, and etc.