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ANGEO | Articles | Volume 36, issue 3
Ann. Geophys., 36, 825–830, 2018
https://doi.org/10.5194/angeo-36-825-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Dynamics and interaction of processes in the Earth and its...

Ann. Geophys., 36, 825–830, 2018
https://doi.org/10.5194/angeo-36-825-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

ANGEO Communicates 06 Jun 2018

ANGEO Communicates | 06 Jun 2018

Seasonal variability of atmospheric tides in the mesosphere and lower thermosphere: meteor radar data and simulations

Dimitry Pokhotelov et al.
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (10 Apr 2018) by Hermann Lühr
AR by Dimitry Pokhotelov on behalf of the Authors (13 Apr 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (18 Apr 2018) by Hermann Lühr
RR by Anonymous Referee #2 (23 Apr 2018)
RR by Anonymous Referee #1 (09 May 2018)
ED: Publish subject to minor revisions (review by editor) (10 May 2018) by Hermann Lühr
AR by Dimitry Pokhotelov on behalf of the Authors (11 May 2018)  Author's response    Manuscript
ED: Publish as is (14 May 2018) by Hermann Lühr
Publications Copernicus
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Short summary
Atmospheric tides are produced by solar heating of the lower atmosphere. The tides propagate to the upper atmosphere and ionosphere playing an important role in the vertical coupling. Ground radar measurements of the seasonal variability of tides are compared with global numerical simulations. The agreement with radar data and limitations of the numerical model are discussed. The work represents a first step in modelling the impact of tidal dynamics on the upper atmosphere and ionosphere.
Atmospheric tides are produced by solar heating of the lower atmosphere. The tides propagate to...
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