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ACP | Articles | Volume 18, issue 17
Atmos. Chem. Phys., 18, 12639–12661, 2018
https://doi.org/10.5194/acp-18-12639-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 18, 12639–12661, 2018
https://doi.org/10.5194/acp-18-12639-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 31 Aug 2018

Research article | 31 Aug 2018

Detection of a climatological short break in the polar night jet in early winter and its relation to cooling over Siberia

Yuta Ando et al.

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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
AR by Yoshihiro Tachibana on behalf of the Authors (09 Mar 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (23 Mar 2018) by Amanda Maycock
RR by Anonymous Referee #1 (01 Apr 2018)
RR by Anonymous Referee #2 (06 Apr 2018)
ED: Publish subject to minor revisions (review by editor) (17 May 2018) by Amanda Maycock
AR by Yoshihiro Tachibana on behalf of the Authors (21 Jun 2018)  Author's response    Manuscript
ED: Publish subject to technical corrections (04 Aug 2018) by Amanda Maycock
AR by Yoshihiro Tachibana on behalf of the Authors (11 Aug 2018)  Author's response    Manuscript
Publications Copernicus
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Short summary
We found the climatological strong stratospheric westerly circumpolar wind stops increasing temporarily during November, when the upward propagation of large-scale atmospheric waves from the troposphere increases. The propagation of atmospheric waves, which is strongest over Siberia, is related to strengthening of the low pressure. Longitudinally asymmetric forcing by land–sea heating contrasts caused by their different heat capacities might cause the strengthening of the low pressure.
We found the climatological strong stratospheric westerly circumpolar wind stops increasing...
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