12 citations as recorded by crossref.

1. Effects of particle precipitation on the polar mesospheric summer echoes observed by EISCAT VHF 224 MHz radar V. Narayanan et al. https://doi.org/10.1016/j.asr.2022.02.015
2. First results of polar mesospheric summer echoes: MARA radar observations from Maitri (70°S), Antarctica R. Rawat et al. https://doi.org/10.1016/j.asr.2025.04.041
3. Influence of Solar and Lunar Tides on the Mesopause Region as Observed in Polar Mesosphere Summer Echoes Characteristics P. Dalin et al. https://doi.org/10.1002/2017JD026509
4. Effects of Energetic Particle Precipitation on PMSE Echoes Observed by EISCAT UHF Radar: A Case Study A. Rauf et al. https://doi.org/10.1134/S0016793222040028
5. Characteristics of PMSE associated with the geomagnetic disturbance driven by corotating interaction region and high‐speed solar wind streams in the declining solar cycle 23 Y. Lee et al. https://doi.org/10.1002/2015JA021144
6. Polar Mesospheric Summer Echo Characteristics in Magnetic Local Time and Height Profiles Y. Lee et al. https://doi.org/10.5140/JASS.2023.40.3.101
7. Tristatic observation of polar mesosphere winter echoes with the EISCAT VHF radar on 8 January 2014: a case study E. Belova et al. https://doi.org/10.1186/s40623-018-0878-5
8. Mid-Latitude Detection of High Schmidt-Number Turbulent Echoes, and Comparison to PMSE and Geomagnetic Variations W. Hocking & V. Pinnegar https://doi.org/10.3390/atmos13030396
9. High-speed solar wind streams and polar mesosphere winter echoes at Troll, Antarctica S. Kirkwood et al. https://doi.org/10.5194/angeo-33-609-2015
10. Ionization and NO production in the polar mesosphere during high-speed solar wind streams: model validation and comparison with NO enhancements observed by Odin-SMR S. Kirkwood et al. https://doi.org/10.5194/angeo-33-561-2015
11. Observation of Polar Mesosphere Summer Echoes using the northernmost MST radar at Eureka (80°N) N. Swarnalingam et al. https://doi.org/10.1016/j.jastp.2017.03.015
12. PMSE dependence on frequency observed simultaneously with VHF and UHF radars in the presence of precipitation S. ULLAH et al. https://doi.org/10.1088/2058-6272/aac8d4