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Gradient
In mathematics and physics, the gradient is a fundamental concept. It represents the direction and rate at which a scalar function experiences the most rapid change in space.
For a multi - variable function
The gradient
The direction of the gradient vector shows the direction in which the function value increases most rapidly, and the magnitude of the gradient indicates the rate of change of the function in that direction.
For instance, in topography, when we consider the terrain height as a function of geographical location (expressed in two - dimensional coordinates), the gradient vector points towards the direction of the steepest upward slope, and the magnitude of the gradient measures how steep this upward slope is.
In coordinate systems, the calculation of the gradient is closely tied to the coordinate system.
The formula for calculating the gradient is:
Let's break down what each term means:
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$U$ : It stands for the principal direction of change. This direction is defined within the local coordinate system$C_u$ . It represents the direction in which the function$f$ changes most significantly. In practical applications, it might be related to the direction of an object's movement, or the direction of a force acting on a system. -
$df$ : This represents the change in the function$f$ . It reflects the amount by which the function value changes in a particular direction. Its value depends on the characteristics of the function$f$ and the specific change scenario being considered. -
$C_u$ : The local coordinate system. It serves as the reference frame for defining the direction$U$ . Different local coordinate systems will lead to different ways of representing the direction$U$ , thereby affecting the result of the gradient calculation. -
$I_c$ : The default world coordinate system. It provides a global reference framework for the entire calculation. All local coordinate systems can be related to and transformed within this world coordinate system. -
$dxyz$ : A vector element defined in the world coordinate system. When multiplied by$I_c$ , it forms a differential coordinate system. This differential coordinate system is crucial for calculating the gradient as it helps us analyze the change of the function within a small, local spatial range.
In actual calculations, to simplify numerical computations, the paper introduces a sufficiently small scaling factor
For example, in some cases, the gradient can be approximated like this:
First, we define
Then,
Here,
By choosing an appropriate differential coordinate system, such as setting