Articles | Volume 17, issue 9
https://doi.org/10.5194/amt-17-2957-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/amt-17-2957-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A new dual-frequency stratospheric–tropospheric and meteor radar: system description and first results
State Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing, 100190, China
Iain Murray Reid
ATRAD Pty. Ltd., 154 Ashley St., Underdale, 5032, Australia
School of Physics, Chemistry and Earth Sciences, The University of Adelaide, Adelaide, 5005, Australia
Bing Cai
State Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing, 100190, China
Christian Adami
ATRAD Pty. Ltd., 154 Ashley St., Underdale, 5032, Australia
Zengmao Zhang
State Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing, 100190, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 100089, China
Mingliang Zhao
State Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing, 100190, China
Wen Li
State Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing, 100190, China
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To capture and characterize the small-scale atmospheric disturbances and dynamics causing by solar activities, an in situ acoustic anemometer has been developed. It is used to obtain wind measurements in the stratosphere on a high altitude balloon in the Stratospheric Environmental respoNses to Solar stORms (SENSOR) campaign. The anemometer is also equipped with sensors to measure temperature, pressure, and relative humidity. Observations were obtained during a flight experiment in 2019.
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Using horizontal wind data collected by the dual-frequency Stratosphere-Troposphere-Meteor radar at the Langfang Observatory, the spatiotemporal characteristics and propagation properties of planetary waves in the troposphere-stratosphere (ST) and mesosphere-lower thermosphere (MLT) were explored, along with their interactions across different atmospheric layers. These new observations enhance our understanding of vertical coupling between the ST and MLT through planetary waves.
Jianyuan Wang, Na Li, Wen Yi, Xianghui Xue, Iain M. Reid, Jianfei Wu, Hailun Ye, Jian Li, Zonghua Ding, Jinsong Chen, Guozhu Li, Yaoyu Tian, Boyuan Chang, Jiajing Wu, and Lei Zhao
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We present the impact of quasi-biennial oscillation (QBO) disruption events on diurnal tides over the low- and mid-latitude MLT region observed by a meteor radar chain. By using a global atmospheric model and reanalysis data, it is found that the stratospheric QBO winds can affect the mesospheric diurnal tides by modulating the subtropical ozone variability in the upper stratosphere and the interaction between tides and gravity waves in the mesosphere.
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Wen Yi, Jie Zeng, Xianghui Xue, Iain Reid, Wei Zhong, Jianfei Wu, Tingdi Chen, and Xiankang Dou
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In recent years, the concept of multistatic meteor radar systems has attracted the attention of the atmospheric radar community, focusing on the MLT region. In this study, we apply a multistatic meteor radar system consisting of a monostatic meteor radar in Mengcheng (33.36° N, 116.49° E) and a remote receiver in Changfeng (31.98° N, 117.22° E) to estimate the two-dimensional horizontal wind field, and the horizontal divergence and relative vorticity of the wind field.
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Preprint withdrawn
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To capture and characterize the small-scale atmospheric disturbances and possible relations to solar activities, an in situ acoustic anemometer has been developed. It is used to obtain wind measurements in the stratosphere on a high altitude balloon in the Stratospheric Environmental respoNses to Solar stORms (SENSOR) campaign. The anemometer is also equipped with sensors to measure temperature, pressure, and relative humidity. Observations were obtained during a flight experiment in 2019.
Joel P. Younger, Iain M. Reid, Chris L. Adami, Chris M. Hall, and Masaki Tsutsumi
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A radar in Svalbard usually used to study meteor trails was used to observe a thin icy layer in the upper atmosphere. New methods used the layer to measure wind speed over short periods of time and found that the layer is most reflective within 6.8 ± 3.3° of vertical. Analysis of meteor trail radar echo durations found that the layer may shorten meteor trail echoes, but more data are needed. This study shows new uses for data collected by meteor radars for other purposes.
Wei Zhong, Xianghui Xue, Wen Yi, Iain M. Reid, Tingdi Chen, and Xiankang Dou
Atmos. Meas. Tech., 14, 3973–3988, https://doi.org/10.5194/amt-14-3973-2021, https://doi.org/10.5194/amt-14-3973-2021, 2021
Song Liang, Hu Xiong, Wei Feng, Yan Zhaoai, Xu Qingchen, and Tu Cui
Atmos. Meas. Tech. Discuss., https://doi.org/10.5194/amt-2021-76, https://doi.org/10.5194/amt-2021-76, 2021
Preprint withdrawn
Short summary
Short summary
To capture and characterize the small-scale atmospheric disturbances and dynamics causing by solar activities, an in situ acoustic anemometer has been developed. It is used to obtain wind measurements in the stratosphere on a high altitude balloon in the Stratospheric Environmental respoNses to Solar stORms (SENSOR) campaign. The anemometer is also equipped with sensors to measure temperature, pressure, and relative humidity. Observations were obtained during a flight experiment in 2019.
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Revised manuscript not accepted
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In this study, we report the climatology of migrating and non-migrating tides in mesopause winds estimated using multiyear observations from three meteor radars in the southern equatorial region. The results reveal that the climatological patterns of tidal amplitudes by meteor radars is similar to the Climatological Tidal Model of the Thermosphere (CTMT) results and the differences are mainly due to the effect of the stratospheric sudden warming (SSW) event.
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Short summary
To have better understanding of the dynamics of the lower and middle atmosphere, we installed a newly designed dual-frequency radar system that uses 53.8 MHz for near-ground to 20 km wind measurements and 35.0 MHz for 70 to 100 km wind measurements. The initial results show its good performance, along with the analysis of typical winter gravity wave activities.
To have better understanding of the dynamics of the lower and middle atmosphere, we installed a...