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5 dni temu · There is rarely any research on landform classification using relative slope position (RSP) and elevation. Therefore, we designed a landform classification method based on RSP and elevation, Terrainforms (TF), and combined the landform type with land use type to construct soil–landscape units for soil type and attribute spatial prediction.
- Classifying Slope Unit by Combining Terrain Feature Lines Based on ...
Accordingly, this paper proposes a novel slope unit...
- Classifying Slope Unit by Combining Terrain Feature Lines Based on ...
17 sie 2018 · Dikau proposed a classification design for 15 classes based on possible combinations of a land slope and a curvature. For tangential curvature (slope area) these classes can only define sloping elements of a surface (Fig. 2 ) and do not have any class features such as channels, ridges and peaks.
6 sty 2023 · Accordingly, this paper proposes a novel slope unit classification method by combining terrain feature lines (CTFL). In this research, the slope units are considered individual slope units formed by the division of terrain feature lines with clear geological significance at the slope scale.
1 kwi 2020 · The proposed approach involves these following four steps: (1) data preparation, (2) DL network building and training, (3) accuracy test and validation, and (4) landform analysis of study area. First, remote sensing imagery, DEMs, and their derivatives were collected as the input dataset.
5 dni temu · The results show that the landform classification method based on RSP and elevation is not easily limited by the analysis scale, and is an efficient and accurate landform classification method.
31 gru 2022 · Landform classification is crucial for a host of applications that include geomorphological, soil mapping, radiative and gravity-controlled processes. Due to the complexity and rapid developments in the field of landform delineation, this study provides a scoping review to identify trends in the field.
2 mar 2023 · Based on the observed field slopes and the dominant geomorphic processes acting on the slope, we created six slope classes, starting from the divide (interfluve), characterized by a lower gradient slope (0–1°), up to the piedmont slope area (e.g. the colluvial footslope), excluding the three ending geomorphological units included in the ...
