Articles | Volume 12, issue 4
https://doi.org/10.5194/esurf-12-863-2024
https://doi.org/10.5194/esurf-12-863-2024
Research article
 | 
17 Jul 2024
Research article |  | 17 Jul 2024

Decadal-scale decay of landslide-derived fluvial suspended sediment after Typhoon Morakot

Gregory A. Ruetenik, Ken L. Ferrier, and Odin Marc

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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 egusphere-2023-1278', Aaron Bufe, 08 Aug 2023
  • RC2: 'Comment on egusphere-2023-1278', Harrison Martin, 08 Jan 2024
  • AC1: 'Comment on egusphere-2023-1278', Gregory Ruetenik, 24 Mar 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Gregory Ruetenik on behalf of the Authors (31 Mar 2024)  Author's response   Author's tracked changes   Manuscript 
EF by Polina Shvedko (04 Apr 2024)  Supplement 
ED: Publish as is (19 Apr 2024) by Kieran Dunne
ED: Publish as is (19 Apr 2024) by Tom Coulthard (Editor)
AR by Gregory Ruetenik on behalf of the Authors (04 May 2024)  Manuscript 
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Short summary
Fluvial sediment fluxes increased dramatically in Taiwan during Typhoon Morakot in 2009, which produced some of the heaviest landsliding on record. We analyzed fluvial discharge and suspended sediment concentration data at 87 gauging stations across Taiwan to quantify fluvial sediment responses since Morakot. In basins heavily impacted by landsliding, rating curve coefficients sharply increased during Morakot and then declined exponentially with a characteristic decay time of <10 years.