2022
DOI: 10.1080/17538947.2022.2088874
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Landform classification based on landform geospatial structure – a case study on Loess Plateau of China

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Cited by 10 publications
(3 citation statements)
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“…DBP is formed by extending the longitudinal profile of the drainage boundary to the plane with the watershed outlet as the focal point. It serves as the highest edge line and the basic skeleton of the basin (Lin et al, 2022c), implying the basic landform evolution process (Condon et al, 2020) and playing a crucial role in driving variations in watershed terrain (Tang et al, 2017). As an erosion‐free zone and overall peripheral structure of the entire basin, DBP is stable and reflects the original geomorphic form of the basin before erosion (Grau Galofre et al, 2018; Liu et al, 2021).…”
Section: Introductionmentioning
confidence: 99%
“…DBP is formed by extending the longitudinal profile of the drainage boundary to the plane with the watershed outlet as the focal point. It serves as the highest edge line and the basic skeleton of the basin (Lin et al, 2022c), implying the basic landform evolution process (Condon et al, 2020) and playing a crucial role in driving variations in watershed terrain (Tang et al, 2017). As an erosion‐free zone and overall peripheral structure of the entire basin, DBP is stable and reflects the original geomorphic form of the basin before erosion (Grau Galofre et al, 2018; Liu et al, 2021).…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, diversified feature selection methods have emerged. Lin et al (2022) measured the importance of terrain features by XGBoost. Zhao et al (2017) constructed a topographic and texture derivatives dataset to quantify terrain features and used the random forest (RF) method to automatically select terrain factors for landform classification tasks.…”
Section: Introductionmentioning
confidence: 99%
“…The surface of the loess hilly regions is full of gullies and complex in structure. The macro wind speed, wind direction, and other meteorological data are constantly evolving under the influence of the gullies on the surface of the loess hilly regions, which makes it easy to produce various types of turbulence and high-speed cyclones [1][2][3]. In most cases, the wind speed, wind direction, and pulsation characteristics are significantly different from the macro meteorological data in strong convective micrometeorology.…”
mentioning
confidence: 99%