Impact of light-absorbing particles on snow albedo darkening and associated radiative forcing over high-mountain Asia: high-resolution WRF-Chem modeling and new satellite observations

Sarangi, Chandan; Qian, Yun; Rittger, Karl; Bormann, Kathryn J.; Liu, Ying; Wang, Hailong; Wan, Hui; Lin, Guangxing; Painter, Thomas H.

doi:https://doi.org/10.5194/acp-19-7105-2019

Articles | Volume 19, issue 10

https://doi.org/10.5194/acp-19-7105-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/acp-19-7105-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 19, issue 10

Research article

|

27 May 2019

Research article |

| 27 May 2019

Impact of light-absorbing particles on snow albedo darkening and associated radiative forcing over high-mountain Asia: high-resolution WRF-Chem modeling and new satellite observations

Chandan Sarangi, Yun Qian, Karl Rittger, Kathryn J. Bormann, Ying Liu, Hailong Wang, Hui Wan, Guangxing Lin, and Thomas H. Painter

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Final revised paper (published on 27 May 2019)
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Preprint (discussion started on 13 Nov 2018)
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Interactive discussion

Status: closed

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

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RC1: 'acp-2018-979', Anonymous Referee #1, 11 Feb 2019
- AC2: 'AC1', Yun Qian, 25 Apr 2019
RC2: 'Review comments on Sarangi et al.', Anonymous Referee #3, 21 Mar 2019
- AC1: 'AC2', Yun Qian, 25 Apr 2019

Peer-review completion

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

AR by Yun Qian on behalf of the Authors (26 Apr 2019) Author's response Manuscript

ED: Publish as is (27 Apr 2019) by Yafang Cheng

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Short summary

Radiative forcing induced by deposition of light-absorbing particles (LAPs) on snow is an important surface forcing. Here, we have used high-resolution WRF-Chem (coupled with online snow–LAP–radiation model) simulations for 2013–2014 to estimate the spatial variation in LAP-induced snow albedo darkening effect in high-mountain Asia. Significant improvement in simulated LAP–snow properties with use of a higher spatial resolution for the same model configuration is illustrated over this region.