Articles | Volume 22, issue 3
Atmos. Chem. Phys., 22, 1921–1937, 2022
https://doi.org/10.5194/acp-22-1921-2022
Atmos. Chem. Phys., 22, 1921–1937, 2022
https://doi.org/10.5194/acp-22-1921-2022

Research article 10 Feb 2022

Research article | 10 Feb 2022

Aerosol radiative impact during the summer 2019 heatwave produced partly by an inter-continental Saharan dust outbreak – Part 2: Long-wave and net dust direct radiative effect

Michaël Sicard et al.

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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 acp-2021-419', Anonymous Referee #1, 25 Oct 2021
  • RC2: 'Comment on acp-2021-419', Anonymous Referee #2, 14 Nov 2021
    • AC2: 'Reply on RC2', Michael Sicard, 09 Dec 2021
  • AC1: 'Reply on RC1', Michael Sicard, 09 Dec 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Michael Sicard on behalf of the Authors (09 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (10 Dec 2021) by Eduardo Landulfo
RR by Anonymous Referee #1 (14 Dec 2021)
RR by Anonymous Referee #2 (04 Jan 2022)
ED: Publish as is (05 Jan 2022) by Eduardo Landulfo
Short summary
This paper completes the companion paper of Córdoba-Jabonero et al. (2021). We estimate the total direct radiative effect produced by mineral dust particles during the June 2019 mega-heatwave at two sites in Spain and Germany. The results show that the dust particles in the atmosphere contribute to cooling the surface (less radiation reaches the surface) and that the heatwave (parametrized by high surface and air temperatures) contributes to reducing this cooling.
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