Determination method for rainstorm-induced shallow landslide disaster warning threshold value
A method for determining rainstorms, applied in forecasting, data processing applications, climate sustainability, etc., can solve problems that affect the accuracy of early warning results and do not consider rainstorm differences
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[0130] (1) Construct the DEM of the target area according to the topographic map data
[0131] The data calculation of the small watershed DEM is carried out on the ARCGIS platform. The main methods of DEM establishment: 1) vectorize 1:10,000 topographic map to establish spatial topological relationship; 2) use triangulated irregular network (TIN) method to convert vector line drawing into TIN data structure for spatial interpolation; 3) Convert the TIN data structure into a grid structure; 4) Resample the grid data to form a grid DEM (GRID format), and generate a small watershed DEM; 5) Interpolate the DEM data to generate contour lines and contour lines The scanned image is color-separated and superimposed, and the generated DEM is checked for gross errors to check whether there is an over-limit offset. The DEM of the study area is attached figure 2 .
[0132] (2) Division of slope units
[0133] Using the DEM generated by the 1:10,000 topographic map as the basis for t...
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