Articles | Volume 18, issue 17
https://doi.org/10.5194/acp-18-12639-2018
https://doi.org/10.5194/acp-18-12639-2018
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, Koji Yamazaki, Yoshihiro Tachibana, Masayo Ogi, and Jinro Ukita

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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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 
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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.
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