Key Laboratory of Mountain Hazards and Surface Processes, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610299, China
Yiduo Liu
Key Laboratory of Mountain Hazards and Surface Processes, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610299, China
Feng Shi
State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
Shanxi Taiyuan Continental Rift Dynamics National Observation and Research Station, Beijing 100029, China
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Total article views: 3,021 (including HTML, PDF, and XML)
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Total article views: 2,542 (including HTML, PDF, and XML)
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Total article views: 479 (including HTML, PDF, and XML)
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The drainage-divide stability provides new insights into both the river network evolution and the tectonic and/or climatic changes. Several methods have been proposed to determine the direction of drainage-divide migration. However, how to quantify the migration rate of drainage divides remains challenging. In this paper, we propose a new method to calculate the migration rate of drainage divides from high-resolution topographic data.
The drainage-divide stability provides new insights into both the river network evolution and...