Variability in individual particle structure and mixing states between the glacier–snowpack and atmosphere in the northeastern Tibetan Plateau

Dong, Zhiwen; Kang, Shichang; Qin, Dahe; Shao, Yaping; Ulbrich, Sven; Qin, Xiang

doi:https://doi.org/10.5194/tc-12-3877-2018

Articles | Volume 12, issue 12

https://doi.org/10.5194/tc-12-3877-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/tc-12-3877-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 12, issue 12

Research article

|

13 Dec 2018

Research article |

| 13 Dec 2018

Variability in individual particle structure and mixing states between the glacier–snowpack and atmosphere in the northeastern Tibetan Plateau

Zhiwen Dong, Shichang Kang, Dahe Qin, Yaping Shao, Sven Ulbrich, and Xiang Qin

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Final revised paper (published on 13 Dec 2018)
Supplement to the final revised paper
Preprint (discussion started on 10 Sep 2018)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review', Anonymous Referee #1, 04 Oct 2018
- AC1: 'Author Response to Anonymous Referee #1', Zhiwen Dong, 26 Nov 2018
RC2: 'Review', Marie Dumont, 08 Oct 2018
- AC2: 'Author Response to # Reviewer 2', Zhiwen Dong, 26 Nov 2018
RC3: 'Review', Jamie L Ward, 13 Oct 2018
- AC3: 'Author Response to # Reviewer 3', Zhiwen Dong, 26 Nov 2018

Peer-review completion

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

AR by Zhiwen Dong on behalf of the Authors (27 Nov 2018) Author's response

ED: Publish as is (02 Dec 2018) by Joel Savarino

Short summary

This study aimed to provide a first and unique record of physicochemical properties and mixing states of LAPs at the glacier and atmosphere interface over the northeastern Tibetan Plateau to determine the individual LAPs' structure aging and mixing state changes through the atmospheric deposition process from atmosphere to glacier–snowpack surface, thereby helping to characterize the LAPs' radiative forcing and climate effects in the cryosphere region.