Articles | Volume 37, issue 4
https://doi.org/10.5194/angeo-37-631-2019
https://doi.org/10.5194/angeo-37-631-2019
Regular paper
 | 
24 Jul 2019
Regular paper |  | 24 Jul 2019

High-resolution Beijing mesosphere–stratosphere–troposphere (MST) radar detection of tropopause structure and variability over Xianghe (39.75° N, 116.96° E), China

Feilong Chen, Gang Chen, Yufang Tian, Shaodong Zhang, Kaiming Huang, Chen Wu, and Weifan Zhang

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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: Reconsider after major revisions (further review by editor and referees) (26 Mar 2019) by Andrew J. Kavanagh
AR by Feilong Chen on behalf of the Authors (28 Mar 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (29 Mar 2019) by Andrew J. Kavanagh
RR by Anonymous Referee #1 (09 May 2019)
RR by Anonymous Referee #2 (14 May 2019)
ED: Publish subject to revisions (further review by editor and referees) (30 May 2019) by Andrew J. Kavanagh
AR by Feilong Chen on behalf of the Authors (21 Jun 2019)  Author's response   Manuscript 
ED: Publish as is (01 Jul 2019) by Andrew J. Kavanagh
AR by Feilong Chen on behalf of the Authors (06 Jul 2019)  Author's response   Manuscript 
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Short summary
Using the Beijing MST radar echo-power observations collected during the period November 2011–May 2017, the structure and variability of the tropopause over Xianghe, China (39.75° N, 116.96° E), was presented. Our comparison results showed a good agreement between the radar and thermal tropopauses during all seasons. In contrast, the consistency between the radar and dynamical tropopauses is poor during summer. Diurnal oscillation in tropopause height is commonly observed during all seasons.