As the topography defines and influences most of the processes that take place in a given terrain, the DEM can be used to extract many different parameters, which give us information about these processes. This recipe shows you how to calculate a popular one, which is called the Topographic wetness index, which estimates the soil wetness based on the topography.
Open the Topographic wetness index algorithm from the Processing Toolbox option and fill it in, as shown in the following screenshot:


The index combines slope and catchment area, two parameters that influence the soil wetness. If the catchment area value is high, this means that more water will flow into the cell, thus, increasing its soil wetness. A low value of slope will have a similar effect because the water that flows into the cell will not flow out of it quickly.
This algorithm expects the slope to be expressed in radians. This is the reason why the Slope, aspect, curvature algorithm has to be used because it produces its slope output in radians. The other Slope algorithm that you will find, which is based on the GDAL library, creates a slope layer with values expressed in degrees. You can use this layer if you convert its units using the raster calculator.