Articles | Volume 22, issue 1
Research article
12 Jan 2022
Research article |  | 12 Jan 2022

Observed slump of sea land breeze in Brisbane under the effect of aerosols from remote transport during 2019 Australian mega fire events

Lixing Shen, Chuanfeng Zhao, Xingchuan Yang, Yikun Yang, and Ping Zhou


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2021-818', Anonymous Referee #1, 13 Oct 2021
    • AC1: 'Reply on RC1', Chuanfeng Zhao, 16 Nov 2021
  • RC2: 'Comment on acp-2021-818', Anonymous Referee #2, 19 Oct 2021
    • AC2: 'Reply on RC2', Chuanfeng Zhao, 16 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Chuanfeng Zhao on behalf of the Authors (16 Nov 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (17 Nov 2021) by Jianping Huang
RR by Anonymous Referee #1 (17 Nov 2021)
ED: Publish as is (06 Dec 2021) by Jianping Huang
Short summary
Using multi-year data, this study reveals the slump of sea land breeze (SLB) at Brisbane during mega fires and investigates the impact of fire-induced aerosols on SLB. Different aerosols have different impacts on sea wind (SW) and land wind (LW). Aerosols cause the decrease of SW, partially offset by the warming effect of black carbon (BC). The large-scale cooling effect of aerosols on sea surface temperature (SST) and the burst of BC contribute to the slump of LW.
Final-revised paper