17 citations as recorded by crossref.

1. Westward Migration of the Chenghai–Jinsha Drainage Divide and Its Implication for the Initiation of the Chenghai Fault S. Bian et al.
2. Eastern Himalayan river captures and upper Assam uplift: Paleo-drainage evolution of the Brahmaputra River P. Rai et al.
3. Channel concavity controls planform complexity of branching drainage networks L. Goren & E. Shelef
4. Drainage rearrangement in an intra-continental mountain belt: a case study from the central South Tian Shan, Kyrgyzstan L. Gong et al.
5. Drainage-divide migration at the Qinling and its implications for the drainage reorganization and rift evolution of the Weihe graben, Central China X. Zeng et al.
6. Record of paleo water divide locations reveals intermittent divide migration and links to paleoclimate proxies E. Harel et al.
7. Recent uplift of Chomolungma enhanced by river drainage piracy X. Han et al.
8. Topographic Response to Horizontal Advection in Normal Fault‐Bound Mountain Ranges A. Hoskins et al.
9. Orographic rainfall drives the Himalaya drainage divide to move north S. Bian et al.
10. Applicability of the landscape evolution model in the absence of rills M. Cheraghi et al.
11. The Yellow River headwater is shrinking in response to the northeastward expansion of the Tibetan Plateau Y. Ye & X. Tan
12. Drainage reorganization induces deviations in the scaling between valley width and drainage area E. Harel et al.
13. How does the newly-formed drainage divide migrate after a river capture event? S. Bian et al.
14. Eastward drainage-divide migrations driven by the spatial variations in precipitation and tectonic uplift contribute to the formation of the Parallel Rivers in the Hengduan Mountains, Southeastern Tibet F. Gao et al.
15. Drainage divide migration and implications for climate and biodiversity C. He et al.
16. Quantifying the migration rate of drainage divides from high-resolution topographic data C. Zhou et al.
17. Late-Quaternary sediments around the wind gap accelerate the wind-gap migration following the Dadu-Anning river capture event Q. Guo et al.