2022
DOI: 10.1086/722362
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Introduction: Redrawing the Map of Science in Modern China

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Cited by 4 publications
(2 citation statements)
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“…Loess geomorphy is the predominant geomorphological type in the Loess Plateau, largely formed through aeolian accumulation and water erosion processes, resulting in unique landforms [33], such as loess tablelands, hills, and ridges, as well as welldeveloped gullies. It is approximately 4~6 km/km 2 , as estimated from 1:50,000 topographic maps [33,34]. Therefore, we selected 13 groups of multi-scale contour clusters of loess geomorphy for this study.…”
Section: Experimental Datasetsmentioning
confidence: 99%
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“…Loess geomorphy is the predominant geomorphological type in the Loess Plateau, largely formed through aeolian accumulation and water erosion processes, resulting in unique landforms [33], such as loess tablelands, hills, and ridges, as well as welldeveloped gullies. It is approximately 4~6 km/km 2 , as estimated from 1:50,000 topographic maps [33,34]. Therefore, we selected 13 groups of multi-scale contour clusters of loess geomorphy for this study.…”
Section: Experimental Datasetsmentioning
confidence: 99%
“…Gully density refers to the lengths of gullies per unit area, and the greater its value, the more the watershed cuts into the geomorphology. Therefore, gully density is one of the most important indicators to represent regional geomorphic features [33], and can be used to measure the distance similarity between valley line hierarchical trees. Due to the fact that the drainage area remains unchanged after contour generalization; therefore, the distance similarity degree (S Dis S 2 S 1…”
Section: Distance Similaritymentioning
confidence: 99%