Modeling dust sources, transport, and radiative effects at different altitudes over the Tibetan Plateau

Hu, Zhiyuan; Huang, Jianping; Zhao, Chun; Jin, Qinjian; Ma, Yuanyuan; Yang, Ben

doi:https://doi.org/10.5194/acp-20-1507-2020

Articles | Volume 20, issue 3

https://doi.org/10.5194/acp-20-1507-2020

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

Special issue:

Study of ozone, aerosols and radiation over the Tibetan Plateau...

https://doi.org/10.5194/acp-20-1507-2020

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

Articles | Volume 20, issue 3

Research article

|

07 Feb 2020

Research article |

| 07 Feb 2020

Modeling dust sources, transport, and radiative effects at different altitudes over the Tibetan Plateau

Zhiyuan Hu, Jianping Huang, Chun Zhao, Qinjian Jin, Yuanyuan Ma, and Ben Yang

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Final revised paper (published on 07 Feb 2020)
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Preprint (discussion started on 07 Aug 2019)
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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: 'referee comments', Anonymous Referee #2, 29 Aug 2019
- AC1: 'Final Response', Zhiyuan Hu, 29 Nov 2019
RC2: 'Comments on "Modeling dust sources, transport, and radiative effects at different altitudes over the Tibetan Plateau"', Anonymous Referee #3, 21 Nov 2019
- AC1: 'Final Response', Zhiyuan Hu, 29 Nov 2019

Peer-review completion

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

AR by Anna Wenzel on behalf of the Authors (05 Dec 2019) Author's response Manuscript

ED: Referee Nomination & Report Request started (06 Dec 2019) by Tao Wang

RR by Anonymous Referee #2 (10 Dec 2019)

RR by Anonymous Referee #3 (21 Dec 2019)

ED: Publish as is (21 Dec 2019) by Tao Wang

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Short summary

This study investigates intercontinental transport of dust plums and distribution characteristics of dust at different altitudes over the Tibetan Plateau (TP). The results show that dust particles are emitted into atmosphere and then transport to the TP. The East Asian dust trasnports southward and is lifted up to the TP in northern slop, while the North Afican dust and Middle East dust transport eastward and concentrate in both northern and southern slops, then is lifted up to the TP.