Articles | Volume 24, issue 22
https://doi.org/10.5194/acp-24-12807-2024
https://doi.org/10.5194/acp-24-12807-2024
Research article
 | 
19 Nov 2024
Research article |  | 19 Nov 2024

Diurnal variation in an amplified canopy urban heat island during heat wave periods in the megacity of Beijing: roles of mountain–valley breeze and urban morphology

Tao Shi, Yuanjian Yang, Ping Qi, and Simone Lolli

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-1200', Anonymous Referee #1, 26 Jun 2024
    • AC1: 'Reply on RC1', Yuanjian Yang, 08 Aug 2024
  • RC2: 'Comment on egusphere-2024-1200', Anonymous Referee #2, 01 Jul 2024
    • AC2: 'Reply on RC2', Yuanjian Yang, 08 Aug 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Yuanjian Yang on behalf of the Authors (08 Aug 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (13 Aug 2024) by Michael Byrne
RR by Anonymous Referee #2 (24 Sep 2024)
ED: Publish as is (25 Sep 2024) by Michael Byrne
AR by Yuanjian Yang on behalf of the Authors (26 Sep 2024)  Manuscript 
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Short summary
This paper explored the formation mechanisms of the amplified canopy urban heat island intensity (ΔCUHII) during heat wave (HW) periods in the megacity of Beijing from the perspectives of mountain–valley breeze and urban morphology. During the mountain breeze phase, high-rise buildings with lower sky view factors (SVFs) had a pronounced effect on the ΔCUHII. During the valley breeze phase, high-rise buildings exerted a dual influence on the ΔCUHII.
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