Articles | Volume 9, issue 5
Earth Surf. Dynam., 9, 1251–1262, 2021
https://doi.org/10.5194/esurf-9-1251-2021
Earth Surf. Dynam., 9, 1251–1262, 2021
https://doi.org/10.5194/esurf-9-1251-2021
Research article
 | Highlight paper
16 Sep 2021
Research article  | Highlight paper | 16 Sep 2021

Landslide-lake outburst floods accelerate downstream hillslope slippage

Wentao Yang 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 esurf-2021-14', Anonymous Referee #1, 08 May 2021
    • AC1: 'Reply on RC1', Wentao Yang, 15 Jun 2021
    • AC2: 'Reply on RC1', Wentao Yang, 15 Jun 2021
  • RC2: 'Comment on esurf-2021-14', Anonymous Referee #2, 10 May 2021
  • EC1: 'AE comment on esurf-2021-14', Jens Turowski, 17 May 2021
    • AC4: 'Reply on EC1', Wentao Yang, 15 Jun 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Wentao Yang on behalf of the Authors (18 Jul 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (19 Jul 2021) by Jens Turowski
RR by Anonymous Referee #1 (30 Jul 2021)
RR by Anonymous Referee #2 (09 Aug 2021)
ED: Publish subject to minor revisions (review by editor) (10 Aug 2021) by Jens Turowski
AR by Wentao Yang on behalf of the Authors (22 Aug 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (24 Aug 2021) by Jens Turowski
ED: Publish subject to technical corrections (29 Aug 2021) by A. Joshua West(Editor)
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Short summary
The eastern Tibetan Plateau is an ideal place to study interactions among different geomorphic drivers. We report the impacts of two 2018 landslide-lake outburst floods up to 100 km distance downstream of the Jinsha River. By using remote sensing images, we found that the 2018 floods caused many hillslopes to slump during the prolonged period afterwards. The finding could help us to obtain a holistic picture of LLF impacts and improve geomorphic models of landscape evolution.