Articles | Volume 23, issue 11
https://doi.org/10.5194/acp-23-6145-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/acp-23-6145-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Variations in global zonal wind from 18 to 100 km due to solar activity and the quasi-biennial oscillation and El Niño–Southern Oscillation during 2002–2019
Institute of Electromagnetic Wave, School of Physics, Henan Normal
University, Xinxiang, 453000, China
State Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing, 100190, China
Jiyao Xu
CORRESPONDING AUTHOR
State Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing, 100190, China
School of Astronomy and Space Science, University of the Chinese Academy of Science, Beijing, 100049, China
Physics Department, Catholic University of America, Washington, DC
20064, USA
NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
Vania F. Andrioli
State Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing, 100190, China
Heliophysics, Planetary Science and Aeronomy Division, National Institute for Space Research (INPE), São José dos Campos, São Paulo, Brazil
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Short summary
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Revised manuscript not accepted
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We presented sharp descent in proton fluxes is accompanied by the corresponding depression of SYM-H index, with a one-to-one correspondence, regardless of the storm intensity in our previous work [Xu et al., 2019]. This paper is a further study of the possible mechanisms, and to quantitified evaluate the effect of full adiabatic changes. Inner belt is not very stable as previous announced especially for the out zone of the inner belt. It is necessary to survey characteristics of protons.
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Short summary
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Short summary
Winds are important in characterizing atmospheric dynamics and coupling. However, it is difficult to directly measure the global winds from the stratosphere to the lower thermosphere. We developed a global zonal wind dataset according to the gradient wind theory and SABER and meteor radar observations. Using the dataset, we studied the intra-annual, inter-annual, and long-term variations. This is helpful to understand the variations and coupling of the stratosphere to the lower thermosphere.
Winds are important in characterizing atmospheric dynamics and coupling. However, it is...
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