A Three-Frequency Ca+ Doppler Lidar for Ion Temperature Measurements in the E and F Regions

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
Fang Wu, Jing Jiao, Lifang Du, Haoran Zheng, Zelong Wang, Xuewu Cheng, Fuju Wu, Yuan Xia, Jiqin Wang, Wei Wang, Kexin Wang, Yuchang Xun, Jiyao Xu, Yajun Zhu, Wei Yuan, Weijun Liu, Guotao Yang
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Abstract

The ion temperature is an important parameter for ionospheric detection, yet there is limited research on ion temperatures at altitude range from 80 to 300 km. Currently, a single-frequency Ca+ ion optical parametric oscillator (OPO) Lidar system can be used to obtain the Ca+ ion density in this region at Yanqing Station, Beijing (40.4°N, 116.0°E). In this study, the ion temperature can be obtained by extending our original lidar to include three-frequency Ca+ Doppler detection. This development represents a pioneering step on measuring ion temperatures by lidar in the ionospheric E-F region. Preliminary results in the E region show that lidar temperatures at 90–105 km under the condition of smooth changes in Ca+ ion morphology align reasonably with satellite-based observations and model-derived temperatures. Additionally, the exploratory ion temperatures of the F layer peak heights at 200–300 km were obtained. Furthermore, parameter optimization and temperature error analysis in the E-F region are explored, providing valuable insights for the development of Ca+ Doppler lidar systems. The advent of Ca+ Doppler lidar has greatly expanded the lidar detection altitude range of temperature and the possibilities for in-depth research on ion temperature and velocity in regions affected by complex electrodynamic effects. These findings lay the foundation for subsequent studies of coupling processes in the ionospheric E-F region.

用于 E 区和 F 区离子温度测量的三频 Ca+ 多普勒激光雷达
离子温度是电离层探测的一个重要参数,但对 80 至 300 公里高度范围内离子温度的研究却很有限。目前,在北京延庆站(北纬40.4°,东经116.0°)使用单频Ca+离子光参量振荡器(OPO)激光雷达系统可以获得该区域的Ca+离子密度。在本研究中,通过对原有激光雷达进行扩展,加入三频 Ca+多普勒探测,可获得离子温度。这一发展标志着在电离层 E-F 区域利用激光雷达测量离子温度迈出了开创性的一步。E 区的初步结果表明,在 Ca+离子形态平稳变化的条件下,90-105 公里处的激光雷达温度与卫星观测结果和模型推导温度相当吻合。此外,还获得了 200-300 公里处 F 层峰高的探索性离子温度。此外,还探讨了 E-F 区域的参数优化和温度误差分析,为 Ca+多普勒激光雷达系统的开发提供了有价值的见解。钙+多普勒激光雷达的出现极大地扩展了激光雷达的温度探测高度范围,为深入研究受复杂电动力学效应影响区域的离子温度和速度提供了可能。这些发现为电离层 E-F 区域耦合过程的后续研究奠定了基础。
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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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