Compositions and mixing states of aerosol particles by aircraft observations in the Arctic springtime, 2018

Adachi, Kouji; Oshima, Naga; Ohata, Sho; Yoshida, Atsushi; Moteki, Nobuhiro; Koike, Makoto

doi:https://doi.org/10.5194/acp-21-3607-2021

Articles | Volume 21, issue 5

https://doi.org/10.5194/acp-21-3607-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/acp-21-3607-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 21, issue 5

Research article

|

09 Mar 2021

Research article |

| 09 Mar 2021

Compositions and mixing states of aerosol particles by aircraft observations in the Arctic springtime, 2018

Kouji Adachi, Naga Oshima, Sho Ohata, Atsushi Yoshida, Nobuhiro Moteki, and Makoto Koike

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Final revised paper (published on 09 Mar 2021)
Supplement to the final revised paper
Preprint (discussion started on 02 Nov 2020)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'Review', Anonymous Referee #1, 21 Nov 2020
RC2: 'Comments on acp-2020-1114', Anonymous Referee #2, 25 Nov 2020
RC3: 'Review for Adachi et al.', Anonymous Referee #3, 08 Dec 2020
AC1: 'Author's replies for all reviewers', Kouji Adachi, 26 Jan 2021

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Kouji Adachi on behalf of the Authors (26 Jan 2021) Author's response Author's tracked changes Manuscript

ED: Publish as is (31 Jan 2021) by Alexander Laskin

AR by Kouji Adachi on behalf of the Authors (01 Feb 2021) Manuscript

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Short summary

Aerosol particles influence the Arctic climate by interacting with solar radiation, forming clouds, and melting surface snow and ice. Individual-particle analyses using transmission electron microscopy (TEM) and model simulations provide evidence of biomass burning and anthropogenic contributions to the Arctic aerosols by showing a wide range of compositions and mixing states depending on sampling altitude. Our results reveal the aerosol aging processes and climate influences in the Arctic.