Articles | Volume 22, issue 8
Atmos. Chem. Phys., 22, 5195–5207, 2022
https://doi.org/10.5194/acp-22-5195-2022
Atmos. Chem. Phys., 22, 5195–5207, 2022
https://doi.org/10.5194/acp-22-5195-2022
Research article
21 Apr 2022
Research article | 21 Apr 2022

In situ observation of warm atmospheric layer and the heat contribution of suspended dust over the Tarim Basin

Chenglong Zhou et al.

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2021-892', Anonymous Referee #2, 21 Nov 2021
    • AC1: 'Reply on RC1', Yuzhi Liu, 10 Jan 2022
  • RC2: 'Comment on acp-2021-892', Anonymous Referee #1, 02 Dec 2021
    • AC2: 'Reply on RC2', Yuzhi Liu, 10 Jan 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Yuzhi Liu on behalf of the Authors (10 Jan 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (09 Feb 2022) by Aijun Ding
RR by Anonymous Referee #2 (17 Feb 2022)
RR by Anonymous Referee #1 (28 Feb 2022)
ED: Publish subject to technical corrections (23 Mar 2022) by Aijun Ding
AR by Yuzhi Liu on behalf of the Authors (24 Mar 2022)  Author's response    Manuscript
Download
Short summary
Based on the radiosonde observations, an anomalously warm layer is measured at altitudes between 500 and 300 hPa over the Tarim Basin (TB) with an average intensity of 2.53 and 1.39 K in the spring and summer, respectively. The heat contributions of dust to this anomalously warm atmospheric layer in spring and summer were 13.77 and 10.25 %, respectively. Topographically, the TB is adjacent to the Tibetan Plateau; we propose the concept of the Tibetan heat source’s northward extension.
Altmetrics
Final-revised paper
Preprint