Cloud condensation nuclei properties of South Asian outflow  over the northern Indian Ocean during winter

Nair, Vijayakumar S.; Jayachandran, Venugopalan Nair; Kompalli, Sobhan Kumar; Gogoi, Mukunda M.; Babu, S. Suresh

doi:https://doi.org/10.5194/acp-20-3135-2020

Articles | Volume 20, issue 5

https://doi.org/10.5194/acp-20-3135-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

Interactions between aerosols and the South West Asian...

https://doi.org/10.5194/acp-20-3135-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 20, issue 5

Research article

|

16 Mar 2020

Research article |

| 16 Mar 2020

Cloud condensation nuclei properties of South Asian outflow over the northern Indian Ocean during winter

Vijayakumar S. Nair, Venugopalan Nair Jayachandran, Sobhan Kumar Kompalli, Mukunda M. Gogoi, and S. Suresh Babu

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Final revised paper (published on 16 Mar 2020)
Preprint (discussion started on 01 Oct 2019)

Interactive discussion

Status: closed

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

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RC1: 'I attached a review', James Hudson, 27 Nov 2019
- AC1: 'Interactive comment on “Cloud Condensation Nuclei properties of South Asian outflow over the northern Indian Ocean during winter” by Vijayakumar S. Nair et al.', Vijayakumar S Nair, 28 Jan 2020
RC2: 'Review comment', Anonymous Referee #2, 08 Jan 2020
- AC2: 'Reply to reviewer comments', Vijayakumar S Nair, 28 Jan 2020

Peer-review completion

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

AR by Vijayakumar S Nair on behalf of the Authors (28 Jan 2020) Author's response Manuscript

ED: Publish as is (05 Feb 2020) by B.V. Krishna Murthy

Short summary

Extensive measurements of the aerosol and cloud condensation nuclei (CCN) properties in South Asian outflow to the northern Indian Ocean were carried out as a part of the ICARB-2018 experiment during winter. At high supersaturations, most of the aerosols in the South Asian outflow become activated as CCN, whereas the aerosol system over the equatorial Indian Ocean is less CCN efficient even at higher supersaturations.