2020
DOI: 10.1007/s12665-020-08986-5
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Karstic conduits and watershed identification based on the morphological characteristics of depressions in the Yunnan–Guizhou Plateau of China

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Cited by 4 publications
(3 citation statements)
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“…Then the depression is reclassified according to the relative depth, whose value is greater than 1 will be assigned to NODATA and the segmentation threshold is set to 1, so as to identify the bottom of the depression, as shown in Figure 2(d). The bottom of an enclosed karst depression can be identified using this method [58].…”
Section: Depression Identification Using Neighborhoodmentioning
confidence: 99%
“…Then the depression is reclassified according to the relative depth, whose value is greater than 1 will be assigned to NODATA and the segmentation threshold is set to 1, so as to identify the bottom of the depression, as shown in Figure 2(d). The bottom of an enclosed karst depression can be identified using this method [58].…”
Section: Depression Identification Using Neighborhoodmentioning
confidence: 99%
“…Therefore, DEM data with a 12.5 m spatial resolution provided by the NASA website (https://urs.earthdata.nasa.gov) were used in this work to identify and extract karst depressions (including negative terrain features such as sinkholes, waterfall holes, BAZIs, artificial negative terrain, etc.) in Guizhou (Figure 2a) with the contour tree method, which was proven to be a very effective method in practice (Miao et al, 2013;Wu et al, 2016;Wang et al, 2017;Yang et al, 2020).…”
Section: Creating An Inventory Of Karst Depressionsmentioning
confidence: 99%
“…South Gombong karst is a range of karst mountains located southwest of Kebumen in Central Java, Indonesia. Karst is characterized by caves, surface drainage, and closed depressions (Yanna et al 2020). As a result, karst has unique qualities and potential that can be utilized.…”
Section: Introductionmentioning
confidence: 99%