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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 33, issue 2
Ann. Geophys., 33, 185–196, 2015
https://doi.org/10.5194/angeo-33-185-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 33, 185–196, 2015
https://doi.org/10.5194/angeo-33-185-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Regular paper 04 Feb 2015

Regular paper | 04 Feb 2015

Tidal signatures of the thermospheric mass density and zonal wind at midlatitude: CHAMP and GRACE observations

C. Xiong1,2, Y.-L. Zhou2, H. Lühr1,2, and S.-Y. Ma2 C. Xiong et al.
  • 1Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
  • 2Department of Space Physics, College of Electronic Information, Wuhan University, 430079 Wuhan, China

Abstract. By using the accelerometer measurements from CHAMP and GRACE satellites, the tidal signatures of the thermospheric mass density and zonal wind at midlatitudes have been analyzed in this study. The results show that the mass density and zonal wind at southern midlatitudes are dominated by a longitudinal wave-1 pattern. The most prominent tidal components in mass density and zonal wind are the diurnal tides D0 and DW2 and the semidiurnal tides SW1 and SW3. This is consistent with the tidal signatures in the F region electron density at midlatitudes as reported by Xiong and Lühr (2014). These same tidal components are observed both in the thermospheric and ionospheric quantities, supporting a mechanism that the non-migrating tides in the upper atmosphere are excited in situ by ion–neutral interactions at midlatitudes, consistent with the modeling results of Jones Jr. et al. (2013). We regard the thermospheric dynamics as the main driver for the electron density tidal structures. An example is the in-phase variation of D0 between electron density and mass density in both hemispheres. Further research including coupled atmospheric models is probably needed for explaining the similarities and differences between thermospheric and ionospheric tidal signals at midlatitudes.

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