Derivatives
Derivatives are the measures you compute directly from the shape of the surface around each cell: how steep it is, which way it faces, and how it bends.
Slope and aspect are the two everyone uses. The twenty one curvature tools that follow describe the bending of the surface in different ways, and they matter for erosion, deposition, water flow and landform analysis.
Start here
Section titled “Start here”Steepness, computed with the Zevenbergen and Thorne method. The single most used terrain derivative, and an input to almost everything else.
| Parameter | What to set |
|---|---|
| Input | Your elevation raster. |
| Units | Degrees, from 0 flat to 90 vertical, the most readable. Percent, the rise over run used in engineering and road design. Radians, for feeding another computation. |
| Z factor | Vertical exaggeration. Leave at 1 when vertical and horizontal units match. |
| Output | The slope raster. |
Slope depends on the resolution of your DEM. The same hillside measured on a 1 metre LiDAR model and on a 30 metre global model will not give the same steepness, because each cell averages a different amount of ground.
Aspect
Section titled “Aspect”The compass direction the slope faces, in degrees: 0 is north, 90 east, 180 south, 270 west. It drives how much sun a slope receives, and with it snow melt, soil moisture and vegetation.
Aspect is circular, which has a practical consequence: 359 and 1 are neighbours, not opposites. Do not average it as an ordinary number, and style it with a cyclic colour scheme so north does not appear twice at both ends of the ramp.
Flat cells have no meaningful aspect.
Plan curvature and Profile curvature
Section titled “Plan curvature and Profile curvature”The two curvatures worth knowing if you never use the others.
Plan curvature measures bending across the slope, at right angles to the flow direction. Positive values mark places where flow converges, which is where water and material concentrate. Negative values mark places where it spreads out.
Profile curvature measures bending along the slope. It tells you where flow accelerates, which is where erosion happens, and where it slows down, which is where material is deposited.
Together they describe the local shape of the ground better than slope alone: a uniform 10 degree hillside and a 10 degree hollow behave very differently.
All the tools
Section titled “All the tools”| Tool | What it does |
|---|---|
| Slope | Steepness in degrees, radians or percent, by the Zevenbergen and Thorne method. |
| Aspect | The compass direction of the steepest descent, in degrees from north. |
| Relative Aspect | Aspect expressed relative to an azimuth you choose, from 0 to 180 degrees. |
| Plan Curvature | Bending across the slope. Positive means converging flow, negative means diverging. |
| Profile Curvature | Bending along the slope. Positive means accelerating flow, negative means decelerating. |
| Tangential Curvature | Lateral curvature perpendicular to the flow line, close to plan curvature but directional. |
| Total Curvature | Overall curvature independent of direction. High at peaks and pits, low on planes. |
| Mean Curvature | Average of the two principal curvatures. Emphasises how smooth or abrupt the surface is. |
| Gaussian Curvature | Product of the principal curvatures. Positive is a bowl or a dome, negative is a saddle, zero is a cylinder. |
| Maximal Curvature | The larger of the two principal curvatures. |
| Minimal Curvature | The smaller of the two principal curvatures. |
| Principal Curvature Direction | The direction, in degrees, in which the surface bends most. |
| Accumulation Curvature | The product of profile and tangential curvature, marking zones of flow accumulation. |
| Casorati Curvature | A single measure of overall bending derived from the principal curvatures. |
| Curvedness | How strongly the surface is curved, regardless of shape. |
| Shape Index | The kind of shape, from cup through saddle to cap, independent of how strongly it curves. |
| Difference Curvature | Half the difference between vertical and horizontal curvature. |
| Generating Function | A combined curvature descriptor used in surface classification. |
| Horizontal Excess Curvature | How much the horizontal curvature exceeds the minimal curvature. |
| Vertical Excess Curvature | How much the vertical curvature exceeds the minimal curvature. |
| Ring Curvature | The squared twisting of flow lines. |
| Rotor | The twisting of flow lines, signed. |
| Unsphericity | Half the difference between the principal curvatures, marking departure from a sphere. |
Curvature values are small. They are expressed per unit of distance, so the raw numbers look like tiny fractions. Style by percentile or with a diverging ramp centred on zero rather than by the raw range.
Smooth first. Curvature amplifies noise, so a LiDAR derived model is usually run through Feature Preserving Smoothing in General before any curvature is computed.
Naming. Whitebox follows the geomorphometric convention where positive plan curvature is convergent. Other software sometimes uses the opposite sign, which is worth remembering when comparing results.