Articles | Volume 24, issue 11
https://doi.org/10.5194/hess-24-5439-2020
https://doi.org/10.5194/hess-24-5439-2020
Research article
 | 
20 Nov 2020
Research article |  | 20 Nov 2020

Accelerated hydrological cycle over the Sanjiangyuan region induces more streamflow extremes at different global warming levels

Peng Ji, Xing Yuan, Feng Ma, and Ming Pan

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Interactive discussion

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: Publish subject to revisions (further review by editor and referees) (28 Sep 2020) by Fuqiang Tian
AR by Xing Yuan on behalf of the Authors (28 Sep 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (04 Oct 2020) by Fuqiang Tian
RR by Anonymous Referee #2 (08 Oct 2020)
RR by Anonymous Referee #1 (09 Oct 2020)
ED: Publish subject to minor revisions (review by editor) (11 Oct 2020) by Fuqiang Tian
AR by Xing Yuan on behalf of the Authors (12 Oct 2020)  Author's response   Manuscript 
ED: Publish as is (13 Oct 2020) by Fuqiang Tian
AR by Xing Yuan on behalf of the Authors (13 Oct 2020)
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Short summary
By performing high-resolution land surface modeling driven by the latest CMIP6 climate models, we find both the dry streamflow extreme over the drought-prone Yellow River headwater and the wet streamflow extreme over the flood-prone Yangtze River headwater will increase under 1.5, 2.0 and 3.0 °C global warming levels and emphasize the importance of considering ecological changes (i.e., vegetation greening and CO2 physiological forcing) in the hydrological projection.