Articles | Volume 22, issue 6
https://doi.org/10.5194/hess-22-3493-2018
https://doi.org/10.5194/hess-22-3493-2018
Research article
 | 
28 Jun 2018
Research article |  | 28 Jun 2018

The temporally varying roles of rainfall, snowmelt and soil moisture for debris flow initiation in a snow-dominated system

Karin Mostbauer, Roland Kaitna, David Prenner, and Markus Hrachowitz

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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: Publish subject to revisions (further review by editor and referees) (14 Jan 2018) by Matjaz Mikos
AR by Karin Mostbauer on behalf of the Authors (12 Feb 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (20 Feb 2018) by Matjaz Mikos
RR by Anonymous Referee #2 (22 Mar 2018)
ED: Publish subject to minor revisions (review by editor) (01 Apr 2018) by Matjaz Mikos
AR by Karin Mostbauer on behalf of the Authors (22 Apr 2018)  Author's response   Manuscript 
ED: Publish as is (24 Apr 2018) by Matjaz Mikos
AR by Karin Mostbauer on behalf of the Authors (28 Apr 2018)
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Short summary
Debris flows represent a severe hazard in mountain regions and so far remain difficult to predict. We applied a hydrological model to link not only precipitation, but also snowmelt, antecedent soil moisture, etc. with debris flow initiation in an Alpine watershed in Austria. Our results highlight the value of this more holistic perspective for developing a better understanding of debris flow initiation.