Articles | Volume 20, issue 10
https://doi.org/10.5194/nhess-20-2739-2020
https://doi.org/10.5194/nhess-20-2739-2020
Research article
 | 
17 Oct 2020
Research article |  | 17 Oct 2020

Annual flood damage influenced by El Niño in the Kan River basin, Iran

Farhad Hooshyaripor, Sanaz Faraji-Ashkavar, Farshad Koohyian, Qiuhong Tang, and Roohollah Noori

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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 (further review by editor and referees) (13 Dec 2019) by Bruno Merz
AR by Roohollah Noori on behalf of the Authors (19 Jan 2020)  Author's response 
ED: Referee Nomination & Report Request started (14 Feb 2020) by Bruno Merz
RR by Xun Sun (25 Feb 2020)
RR by Anonymous Referee #2 (09 Mar 2020)
ED: Reconsider after major revisions (further review by editor and referees) (15 Mar 2020) by Bruno Merz
AR by Roohollah Noori on behalf of the Authors (06 May 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (11 May 2020) by Bruno Merz
RR by Anonymous Referee #2 (24 May 2020)
ED: Reconsider after major revisions (further review by editor and referees) (02 Jun 2020) by Bruno Merz
AR by Roohollah Noori on behalf of the Authors (14 Jul 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (28 Jul 2020) by Bruno Merz
RR by Anonymous Referee #2 (19 Aug 2020)
ED: Publish subject to technical corrections (19 Aug 2020) by Bruno Merz
AR by Roohollah Noori on behalf of the Authors (27 Aug 2020)  Author's response   Manuscript 
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Short summary
The effect of El Niño on flood damage was investigated. The methodology was based on the calculation of increasing rainfall amount during El Niño events compared to normal conditions. With the southern oscillation index equal to −1.0 as the threshold of El Niño, the annual percentage of increased rainfall is 12.2 %. The annual change factor may not necessarily be transferred to extreme values. Nonetheless, the change factor was applied for generating simulated storms of different return periods.
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