Articles | Volume 20, issue 7
https://doi.org/10.5194/hess-20-3027-2016
https://doi.org/10.5194/hess-20-3027-2016
Research article
 | 
29 Jul 2016
Research article |  | 29 Jul 2016

Mekong River flow and hydrological extremes under climate change

Long Phi Hoang, Hannu Lauri, Matti Kummu, Jorma Koponen, Michelle T. H. van Vliet, Iwan Supit, Rik Leemans, Pavel Kabat, and Fulco Ludwig

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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: Reconsider after major revisions (07 Mar 2016) by Fuqiang Tian
AR by Long Hoang on behalf of the Authors (01 Apr 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (11 Apr 2016) by Fuqiang Tian
RR by Anonymous Referee #1 (02 May 2016)
RR by Anonymous Referee #3 (16 May 2016)
ED: Publish subject to minor revisions (Editor review) (31 May 2016) by Fuqiang Tian
AR by Long Hoang on behalf of the Authors (10 Jun 2016)  Author's response   Manuscript 
ED: Publish as is (29 Jun 2016) by Fuqiang Tian
AR by Long Hoang on behalf of the Authors (04 Jul 2016)
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Short summary
We modelled hydrological changes under climate change in the Mekong River, focusing on extreme events. The scenario ensemble shows an intensification of the hydrological cycle under climate change. Annual river flow increases between 5 and 16 % depending on locations. Extreme high flows increase substantially in both magnitude and frequency, posing threats to flood safety in the basin. Extreme low-flow events are projected to reduce as a result of increased river flow during the dry season.