Articles | Volume 20, issue 13
Atmos. Chem. Phys., 20, 8139–8156, 2020

Special issue: Arctic mixed-phase clouds as studied during the ACLOUD/PASCAL...

Atmos. Chem. Phys., 20, 8139–8156, 2020

Research article 13 Jul 2020

Research article | 13 Jul 2020

Combining atmospheric and snow radiative transfer models to assess the solar radiative effects of black carbon in the Arctic

Tobias Donth et al.


Interactive discussion

Status: closed
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
AR by Evelyn Jäkel on behalf of the Authors (15 Jun 2020)  Author's response    Manuscript
ED: Publish as is (18 Jun 2020) by Jost Heintzenberg
Short summary
Solar radiative effects of Arctic black carbon (BC) particles (suspended in the atmosphere and in the surface snowpack) were quantified under cloudless and cloudy conditions. An atmospheric and a snow radiative transfer model were coupled to account for radiative interactions between both compartments. It was found that (i) the warming effect of BC in the snowpack overcompensates for the atmospheric BC cooling effect, and (ii) clouds tend to reduce the atmospheric BC cooling and snow BC warming.
Final-revised paper