forked from BilalY/Rasagar
41 lines
4.2 KiB
Markdown
41 lines
4.2 KiB
Markdown
# Wind Erosion
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Select a Terrain tile to bring up the Terrain Inspector. In the Terrain Inspector, click the **Paint Terrain** icon, and select **Erosion** > **Wind** from the list of Terrain tools.
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![Wind erosion tool being selected from the inspector](images/2-33-Wind-Erosion-01.png)
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Alternatively, select the terrain, and select the wind erosion icon on the terrain toolbar.
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![Wind Icon](images/Icons/WindErosion.png)
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The Wind Erosion Tool simulates the effect of wind transporting and redistributing sediment.
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The Wind Erosion Tool uses a smooth rotation jitter control, which is slightly different from the standard rotation control. Instead of computing a random rotation value for each frame, this tool uses a smooth noise function to simulate gradual changes in wind direction. Use the **Jitter** slider in the **Brush Rotation** section of the [Common Brush controls](brush-controls-shortcut-keys.md) to control the frequency of these rotation changes.
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The erosion effect depends on the Terrain size and heightmap resolution. For highly detailed erosion features, use a Terrain heightmap resolution of 1025 or greater.
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## Parameters
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![Wind erosion tool control parameters](images/2-33-Wind-Erosion-02.png)
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| **Property** | | **Description** |
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| ---- | ---- | ---- |
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| **Simulation Scale** | | The scale of the simulation, which controls the size of features that erosion produces. Increasing this value results in smoother features, and decreasing it produces higher frequency details. |
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| **Wind Speed** | | The wind speed at the start of the simulation. Higher wind speeds result in a greater visual effect, but might lead to simulation instabilities. |
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| **Advanced** | | |
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|| **Time Interval (dt)** | The time delta for each iteration of the erosion simulation. Higher numbers result in a greater visible effect, but values that are too high can cause simulation instability and inaccuracies. |
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|| **Iterations** | The number of simulation iterations to perform for each Brush stamp. Higher numbers produce more realistic results, but at the cost of performance. |
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|| **Particle Suspension Rate** | The rate at which the simulation removes sediment particles from the Terrain height. |
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|| **Particle Deposit Rate** | The rate at which the simulation deposits sediment particles onto the Terrain height. |
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|| **Slope Factor** | The degree to which the Terrain slope affects sediment suspension. The simulation removes more sediment from surfaces that are more perpendicular to the wind angle.Examples:0 - No effect based on the slope of the Terrain.1 - Full effect based on the slope of the Terrain. |
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|| **Flow Rate** | The rate at which suspended sediment particles travel through the wind flow field. Set this value higher to make sediment travel further and faster. |
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|| **Drag** | The drag coefficient for the wind flow field. Increasing this value will dampen the wind velocity, which results in a smoother effect. |
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|| **Surface Reflection** | The degree to which wind velocities bounce off steep surfaces. |
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|| **Diffusion Rate** | The rate at which suspended sediment diffuses throughout the wind flow field. |
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|| **Abrasiveness** | The rate at which suspended sediment particles erode the Terrain height. |
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|| **Viscosity** | The density of the air, which affects wind fluidity. Higher values slow down the speed of the wind across the Terrain, because the air is thicker. |
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| **Thermal Smoothing** | | After the wind erosion step, you can perform a few iterations of thermal erosion to smooth the Terrain by changing the following parameters. |
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|| **# Iterations** | The number of thermal smoothing iterations to perform. Increasing this results in higher quality thermal smoothing at the expense of performance. |
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|| **dt Scalar** | A multiplier on the time interval to use for thermal smoothing. Increasing this value results in a great smoothing effect, but might lead to simulation instabilities. |
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|| **Resting Angle** | The angle of repose (talus angle). Slopes steeper than this angle are smoothed down until they meet this threshold. |
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