Articles | Volume 22, issue 2
Nat. Hazards Earth Syst. Sci., 22, 377–393, 2022
https://doi.org/10.5194/nhess-22-377-2022
Nat. Hazards Earth Syst. Sci., 22, 377–393, 2022
https://doi.org/10.5194/nhess-22-377-2022

Research article 10 Feb 2022

Research article | 10 Feb 2022

A modeling methodology to study the tributary-junction alluvial fan connectivity during a debris flow event

Alex Garcés et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on nhess-2021-266', Anonymous Referee #1, 05 Oct 2021
    • AC1: 'Reply on RC1', Alex Garces, 09 Nov 2021
  • RC2: 'Comment on nhess-2021-266', Eric Barefoot, 28 Oct 2021
    • AC2: 'Reply on RC2', Alex Garces, 20 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (30 Nov 2021) by Paola Reichenbach
AR by Alex Garces on behalf of the Authors (10 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (15 Dec 2021) by Paola Reichenbach
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Short summary
We propose a workflow to model the response of an alluvial fan located in the Atacama Desert during an extreme storm event. For this alluvial fan, five different deposits were identified and associated with different debris flow surges. Using a commercial software program, our workflow concatenates these surges into one model. This study depicts the significance of the mechanical classification of debris flows to reproduce how an alluvial fan controls the tributary–river junction connectivity.
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