Critical scales to explain urban hydrological response: an application in Cranbrook, London

Cristiano, Elena; ten Veldhuis, Marie-Claire; Gaitan, Santiago; Ochoa Rodriguez, Susana; van de Giesen, Nick

doi:https://doi.org/10.5194/hess-22-2425-2018

Articles | Volume 22, issue 4

https://doi.org/10.5194/hess-22-2425-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/hess-22-2425-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 22, issue 4

Research article

|

23 Apr 2018

Research article |

| 23 Apr 2018

Critical scales to explain urban hydrological response: an application in Cranbrook, London

Elena Cristiano, Marie-Claire ten Veldhuis, Santiago Gaitan, Susana Ochoa Rodriguez, and Nick van de Giesen

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Final revised paper (published on 23 Apr 2018)
Supplement to the final revised paper
Preprint (discussion started on 09 Jan 2018)
Supplement to the preprint

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

SC1: 'Data location mismatch', Anne Jefferson, 08 Feb 2018
- AC1: 'Reply to Anne Jefferson', Elena Cristiano, 26 Feb 2018
RC1: 'Review', Kristian Förster, 09 Feb 2018
- AC2: 'Reply to Kristian Förster', Elena Cristiano, 26 Feb 2018
RC2: 'Reviewer comments', Anonymous Referee #2, 13 Feb 2018
- AC3: 'Reply Anonymous Referee #2', Elena Cristiano, 02 Mar 2018

Peer-review completion

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

ED: Publish subject to minor revisions (review by editor) (16 Mar 2018) by Markus Weiler

AR by Elena Cristiano on behalf of the Authors (23 Mar 2018) Author's response Manuscript

ED: Publish as is (02 Apr 2018) by Markus Weiler

AR by Elena Cristiano on behalf of the Authors (05 Apr 2018)

Short summary

In this work we investigate the influence rainfall and catchment scales have on hydrological response. This problem is quite relevant in urban areas, where the response is fast due to the high degree of imperviousness. We presented a new approach to classify rainfall variability in space and time and use this classification to investigate rainfall aggregation effects on urban hydrological response. This classification allows the spatial extension of the main core of the storm to be identified.