Articles | Volume 20, issue 18
Atmos. Chem. Phys., 20, 10911–10935, 2020
https://doi.org/10.5194/acp-20-10911-2020
Atmos. Chem. Phys., 20, 10911–10935, 2020
https://doi.org/10.5194/acp-20-10911-2020

Research article 22 Sep 2020

Research article | 22 Sep 2020

Examining the atmospheric radiative and snow-darkening effects of black carbon and dust across the Rocky Mountains of the United States using WRF-Chem

Stefan Rahimi et al.

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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 Stefan Rahimi-Esfarjani on behalf of the Authors (19 Jun 2020)  Author's response
ED: Referee Nomination & Report Request started (07 Jul 2020) by Federico Fierli
RR by Hans-Werner Jacobi (17 Jul 2020)
RR by Anonymous Referee #2 (26 Jul 2020)
ED: Publish subject to technical corrections (07 Aug 2020) by Federico Fierli
AR by Stefan Rahimi-Esfarjani on behalf of the Authors (11 Aug 2020)  Author's response    Manuscript
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Short summary
Dark particles emitted to the atmosphere can absorb sunlight and heat the air. As these particles settle, they may darken the surface, especially over snow-covered regions like the Rocky Mountains. This darkening of the surface may lead to changes in snowpack, affecting the local meteorology and hydrology. We seek to evaluate whether these light-absorbing particles more prominently affect this region through their atmospheric presence or their on-snow presence.
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