Effects and consideration of storm movement in rainfall&ndash;runoff modelling at the basin scale

Sigaroodi, Shahram Khalighi; Chen, Qiuwen

doi:https://doi.org/10.5194/hess-20-5063-2016

Articles | Volume 20, issue 12

https://doi.org/10.5194/hess-20-5063-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue:

Modeling hydrological processes and changes

https://doi.org/10.5194/hess-20-5063-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 20, issue 12

Research article

|

21 Dec 2016

Research article |

| 21 Dec 2016

Effects and consideration of storm movement in rainfall–runoff modelling at the basin scale

Shahram Khalighi Sigaroodi and Qiuwen Chen

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Final revised paper (published on 21 Dec 2016)
Supplement to the final revised paper
Preprint (discussion started on 07 Sep 2016)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC1: 'Study on the effects of storm movement on rainfall-runoff modelling at the basin scale', Guoqiang Wang, 22 Sep 2016
- AC1: 'Response to reviewer 1', Qiuwen Chen, 20 Oct 2016
RC2: 'review report', Anonymous Referee #2, 04 Oct 2016
- AC2: 'Response to reviewer 2', Qiuwen Chen, 21 Oct 2016
- AC4: 'Revised figures', Qiuwen Chen, 21 Oct 2016
AC3: 'Revised manuscript and figures', Qiuwen Chen, 21 Oct 2016

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to revisions (further review by Editor and Referees) (10 Nov 2016) by Yaning Chen

AR by Qiuwen Chen on behalf of the Authors (25 Nov 2016) Author's response Manuscript

ED: Publish as is (29 Nov 2016) by Yaning Chen

Short summary

The paper presents original research about storm movement effects on runoff modelling at the basin scale instead of the conventional laboratory scale. It is essential to find that neglecting storm movement may bring artifacts to parameters when calibrating hydrological models; slow movement of storm has a more significant effect on hydrograph; storm movement on hydrograph modelling becomes visible only when the study area is divided into sub-basins.