Case analysis of diurnal stratospheric Rayleigh temperature and atmospheric fluctuations based on 589 nm lidarOA
Case analysis of diurnal stratospheric Rayleigh temperature and atmospheric fluctuations based on 589 nm lidar
ZhiFang Chen;ZhaoAi Yan;Xiong Hu;WenJie Guo;ZunJie Wu;HaiLong Sun;ShangYong Guo;YongQiang Cheng
State Key Laboratory of Solar Activity and Space Weather,National Space Science Center,Chinese Academy of Sciences,Beijing 100190,China||University of Chinese Academy of Sciences,Beijing 100049,ChinaState Key Laboratory of Solar Activity and Space Weather,National Space Science Center,Chinese Academy of Sciences,Beijing 100190,China||University of Chinese Academy of Sciences,Beijing 100049,ChinaState Key Laboratory of Solar Activity and Space Weather,National Space Science Center,Chinese Academy of Sciences,Beijing 100190,ChinaState Key Laboratory of Solar Activity and Space Weather,National Space Science Center,Chinese Academy of Sciences,Beijing 100190,ChinaState Key Laboratory of Solar Activity and Space Weather,National Space Science Center,Chinese Academy of Sciences,Beijing 100190,China||University of Chinese Academy of Sciences,Beijing 100049,ChinaState Key Laboratory of Solar Activity and Space Weather,National Space Science Center,Chinese Academy of Sciences,Beijing 100190,ChinaState Key Laboratory of Solar Activity and Space Weather,National Space Science Center,Chinese Academy of Sciences,Beijing 100190,ChinaState Key Laboratory of Solar Activity and Space Weather,National Space Science Center,Chinese Academy of Sciences,Beijing 100190,China
stratosphereatmospheric temperaturequasi-monochromatic inertial gravity wavevertical wavelengthperiodatmospheric tidal wave
stratosphereatmospheric temperaturequasi-monochromatic inertial gravity wavevertical wavelengthperiodatmospheric tidal wave
《地球与行星物理（英文）》 2026 (2)
251-258,8
This study was supported by the Key Research Program of the Chinese Academy of Sciences(Grant NO.KGFZD-145-23-17)and the Specialized Research Fund for State Key Laboratories.We also acknowledge the use of the ERA5 reanalysis data from the European Centre for Medium-Range Weather Forecastsrelevant data can be accessed from https://cds.climate.copernicus.eu/datasets/reanalysis-era5-complete?tab=d_download.
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