Articles | Volume 19, issue 10
https://doi.org/10.5194/nhess-19-2281-2019
https://doi.org/10.5194/nhess-19-2281-2019
Research article
 | 
17 Oct 2019
Research article |  | 17 Oct 2019

Identifying a transition climate zone in an arid river basin using the evaporative stress index

Yongqiang Liu, Lu Hao, Decheng Zhou, Cen Pan, Peilong Liu, Zhe Xiong, and Ge Sun

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (27 Jul 2018) by Kai Schröter
AR by Yongqiang Liu on behalf of the Authors (07 Sep 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (21 Sep 2018) by Kai Schröter
RR by Anonymous Referee #1 (10 Oct 2018)
RR by Anonymous Referee #3 (31 May 2019)
ED: Reconsider after major revisions (further review by editor and referees) (24 Jun 2019) by Kai Schröter
AR by Yongqiang Liu on behalf of the Authors (05 Aug 2019)  Manuscript 
ED: Referee Nomination & Report Request started (08 Aug 2019) by Kai Schröter
RR by Anonymous Referee #3 (06 Sep 2019)
ED: Publish subject to technical corrections (06 Sep 2019) by Kai Schröter
AR by Yongqiang Liu on behalf of the Authors (09 Sep 2019)  Author's response   Manuscript 
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Short summary
A transition zone often exists between a moist upper river reach and an arid lower reach in a watershed with complex topography. This zone is more suitable for human activities but is difficult to identify in climate classification. We found that a hydrological index overpowers a meteorological index in identifying a transition zone of a watershed in northwestern China, indicating the important role of the land-surface processes and human disturbances in formulating the transition zone.
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