Articles | Volume 24, issue 8
https://doi.org/10.5194/hess-24-4169-2020
https://doi.org/10.5194/hess-24-4169-2020
Research article
 | 
26 Aug 2020
Research article |  | 26 Aug 2020

Hydrological and runoff formation processes based on isotope tracing during ablation period in the source regions of Yangtze River

Zong-Jie Li, Zong-Xing Li, Ling-Ling Song, Juan Gui, Jian Xue, Bai Juan Zhang, and Wen De Gao

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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (17 Jan 2020) by Fuqiang Tian
AR by li zongjie on behalf of the Authors (24 Apr 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (23 May 2020) by Fuqiang Tian
RR by Anonymous Referee #1 (16 Jun 2020)
RR by Anonymous Referee #2 (20 Jun 2020)
ED: Publish as is (02 Jul 2020) by Fuqiang Tian
AR by li zongjie on behalf of the Authors (09 Jul 2020)  Manuscript 
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Short summary
This study mainly explores the hydraulic relations, recharge–drainage relations and their transformation paths, and the processes of each water body. It determines the composition of runoff, quantifies the contribution of each runoff component to different types of tributaries, and analyzes the hydrological effects of the temporal and spatial variation in runoff components. More importantly, we discuss the hydrological significance of permafrost and hydrological processes.