30 Mar 2023
 | 30 Mar 2023
Status: a revised version of this preprint is currently under review for the journal ESurf.

Knickpoints and Fixpoints: The Evolution of Fluvial Morphology under the Combined Effect of Fault Uplift and Dam Obstruction on a Soft Bedrock River

Hung-En Chen, Yen-Yu Chiu, Chih-Yuan Cheng, and Su-Chin Chen

Abstract. Rapid changes in river geomorphology can occur after being disturbed by external factors like earthquakes or large dam obstructions. Studies documenting the evolution of river morphology under such conditions have advanced our understanding of fluvial geomorphology. The Dajia River in Taiwan presents a unique example of the combined effects of a coseismic fault (the 1999 Mw 7.6 Chi-Chi earthquake) and a dam. As a result of the steep terrain and abundant precipitation, rivers in Taiwan have exhibited characteristic post-disturbance evolution over 20 years. This study also considers two other comparative rivers with similar congenital conditions: the Daan River was affected by a thrust fault Chi-Chi earthquake, too; the Zhuoshui River was influenced by dam construction finished in 2001. The survey data and knickpoint migration model were used to analyze the evolution of the three rivers and propose hypothesis models. Results showed that the mobile knickpoint migrated upstream under the influence of flow, while the dam acted as a fixpoint, leading to an increased elevation gap and downstream channel incision. Thereby, the Dajia river narrowing and incision began at both ends and progressively spread to the whole reach under the combined effects.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Hung-En Chen, Yen-Yu Chiu, Chih-Yuan Cheng, and Su-Chin Chen

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on esurf-2023-8', Anonymous Referee #1, 22 May 2023
    • AC1: 'Reply on RC1', Su-Chin Chen, 03 Aug 2023
  • RC2: 'Comment on esurf-2023-8', Anonymous Referee #2, 27 Jun 2023
    • AC2: 'Reply on RC2', Su-Chin Chen, 03 Aug 2023
Hung-En Chen, Yen-Yu Chiu, Chih-Yuan Cheng, and Su-Chin Chen
Hung-En Chen, Yen-Yu Chiu, Chih-Yuan Cheng, and Su-Chin Chen


Total article views: 792 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
559 198 35 792 27 25
  • HTML: 559
  • PDF: 198
  • XML: 35
  • Total: 792
  • BibTeX: 27
  • EndNote: 25
Views and downloads (calculated since 30 Mar 2023)
Cumulative views and downloads (calculated since 30 Mar 2023)

Viewed (geographical distribution)

Total article views: 773 (including HTML, PDF, and XML) Thereof 773 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
Latest update: 15 Jul 2024
Short summary
This study explores the fluvial morphology evolution in three rivers in Taiwan caused by natural tectonic movements (the 1999 Mw 7.6 Chi-Chi earthquake) and human-made structures (Dams). Knickpoints resulting from riverbed uplift move, leading to gradual evolution from instability to equilibrium. Dams, on the other hand, cause continuous degradation of the bed. When both effects exist on a reach, the impact of the knickpoint gradually fades away, but the results of the dam on the river persist.