Articles | Volume 17, issue 11
https://doi.org/10.5194/nhess-17-1923-2017
https://doi.org/10.5194/nhess-17-1923-2017
Research article
 | 
14 Nov 2017
Research article |  | 14 Nov 2017

Relationship between the accumulation of sediment storage and debris-flow characteristics in a debris-flow initiation zone, Ohya landslide body, Japan

Fumitoshi Imaizumi, Yuichi S. Hayakawa, Norifumi Hotta, Haruka Tsunetaka, Okihiro Ohsaka, and Satoshi Tsuchiya

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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) (21 Apr 2017) by Paolo Tarolli
AR by Fumitoshi Imaizumi on behalf of the Authors (12 May 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (16 May 2017) by Paolo Tarolli
RR by Carlo Gregoretti (06 Jun 2017)
RR by Michel Jaboyedoff (03 Jul 2017)
RR by Anonymous Referee #3 (06 Jul 2017)
ED: Reconsider after major revisions (further review by Editor and Referees) (17 Jul 2017) by Paolo Tarolli
AR by Fumitoshi Imaizumi on behalf of the Authors (28 Aug 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (29 Aug 2017) by Paolo Tarolli
RR by Carlo Gregoretti (11 Sep 2017)
ED: Publish subject to minor revisions (further review by Editor) (26 Sep 2017) by Paolo Tarolli
AR by Fumitoshi Imaizumi on behalf of the Authors (06 Oct 2017)  Author's response   Manuscript 
ED: Publish as is (11 Oct 2017) by Paolo Tarolli
AR by Fumitoshi Imaizumi on behalf of the Authors (12 Oct 2017)
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Short summary
Debris flow characteristics in the initiation zones are poorly understood because of the difficulty in monitoring. We studied the relationship between the flow characteristics and the accumulation conditions of the storage in an initiation zone of debris flow. Our study clarified that both partly and fully saturated flows are important processes in the initiation zones of debris flow. The predominant type of flow varied temporally and was affected by the volume of storage and rainfall patterns.
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