Dominance of climate warming effects on recent drying trends over wet monsoon regions

Park, Chang-Eui; Jeong, Su-Jong; Ho, Chang-Hoi; Park, Hoonyoung; Piao, Shilong; Kim, Jinwon; Feng, Song

doi:https://doi.org/10.5194/acp-17-10467-2017

Articles | Volume 17, issue 17

https://doi.org/10.5194/acp-17-10467-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-17-10467-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 17, issue 17

Research article

|

07 Sep 2017

Research article |

| 07 Sep 2017

Dominance of climate warming effects on recent drying trends over wet monsoon regions

Chang-Eui Park, Su-Jong Jeong, Chang-Hoi Ho, Hoonyoung Park, Shilong Piao, Jinwon Kim, and Song Feng

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Final revised paper (published on 07 Sep 2017)
Supplement to the final revised paper
Preprint (discussion started on 14 Feb 2017)
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: 'comments', Anonymous Referee #1, 18 Feb 2017
- AC1: 'Reply to comments', Su-Jong Jeong, 10 Mar 2017
- RC2: 'Review Comments', Anonymous Referee #2, 10 Jul 2017
  - AC2: 'Reply to Review comments', Su-Jong Jeong, 18 Jul 2017

Peer-review completion

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

AR by Su-Jong Jeong on behalf of the Authors (05 Aug 2017) Author's response Manuscript

ED: Publish as is (08 Aug 2017) by Timothy Garrett

AR by Su-Jong Jeong on behalf of the Authors (08 Aug 2017)

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Short summary

In dry monsoon regions, a decrease in precipitation induces drying trends. In contrast, the increase in potential evapotranspiration due to increased atmospheric water-holding capacity, a secondary impact of warming, works to increase aridity over the humid monsoon regions despite the increase in precipitation. Our results explain the recent drying in the humid monsoon regions. This also supports the drying trends over the warm and water-sufficient regions in future climate.