An Enhanced Steepest Descent Method for Global Optimization-Based Mesh Smoothing

Abstract

In order to speed up the global optimization-based mesh smoothing, an enhanced steepest descent method is presented in the paper. Numerical experiment results show that the method performs better than the steepest descent method in the global smoothing. We also presented a physically-based interpretation to explain why the method works better than the steepest descent method.

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Zhao, K. , Ma, Y. , Wang, Y. , Yin, X. and Guo, Y. (2020) An Enhanced Steepest Descent Method for Global Optimization-Based Mesh Smoothing. Journal of Applied Mathematics and Physics, 8, 2509-2518. doi: 10.4236/jamp.2020.811186.

1. Introduction

Mesh quality is import for the finite element method. Mesh with high quality can reduce the time to solution, and increase the solution accuracy [1] [2]. Therefore, mesh quality improvement methods are often used in the mesh generation [3] [4]. There are three types of mesh improvement methods: node insertion/deletion optimization [5] [6] [7], topological optimization [8] [9] [10] [11] and geometrical optimization [12]-[23]. Geometrical optimization is also called smoothing, since it improves the mesh by relocating mesh vertices, while preserving mesh topology. For this reason, smoothing has an important role in mesh optimization.

Laplacian smoothing and optimization-based smoothing are two main smoothing methods. Laplacian smoothing method is very efficient, since it calculates the node movements straightforward. But its optimization performance is not as good as optimization-based smoothing, and it may even result in some invalid elements. Some variations of Laplacian smoothing are presented in order to overcome these disadvantages. Smart Laplacian smoothing is one commonly used variation [14] [24]. Other variations are based on geometric element transformation [16] [17] [19] [25] or angle improvement [15]. Optimization-based smoothing method uses mesh quality to define a cost function, then treats the mesh optimization problem as a cost minimisation problem [26]. Optimization-based smoothing can avoid bad elements and obtain a higher quality mesh. However, its computational cost is higher.

There is a famous optimization-based smoothing Toolkit called Mesquite [27]. Its solver methods include steepest descent method, conjugate gradient method, quasi-Newton method, trust region method, and feasible Newton method [28] [29]. The steepest descent method and the conjugate gradient method are gradient-based, whereas the remaining three are Hessian-based.

Optimization-based smoothing can be divided into global optimization-based smoothing and local optimization-based smoothing. The global smoothing is an all-vertex method where the positions of all free vertices are moved simultaneously within a single iteration, and the local smoothing is a single-vertex method where the position of only one vertex is modified at a time. The performance of the global optimization-based smoothing is better than that of the local optimization-based smoothing [29] [30]. However, the number of variables for global smoothing is proportional to the mesh node number. With the increasing of the mesh nodes, the Hessian-based methods are more unsuitable for global smoothing. Thus, the gradient-based methods appear to be dominant in the global optimization-based smoothing. The conjugate gradient method has been shown to be superior to the steepest descent in most applications [31]. However, the conjugate gradient method requires more storage of intermediate results and more computational cost in a single iteration than the steepest descent method. In addition, the conjugate gradient method is less robust where the cost function surface is relatively flat [32].

Therefore, improving performance of the steepest descent method will facilitate the global optimization-based smoothing. We presented a method which works better than the steepest descent method, but with same storage and almost negligible added computational cost.

The rest of the paper is organized as follows. In Section 2, we briefly review the steepest descent method and point out its shortcomings in mesh optimization. In Section 3, we describe the enhanced steepest descent method and present a physically-based interpretation to explain why the method works better than the steepest descent method. In Section 4, some numerical experiments for triangular meshes and tetrahedral meshes with different initial configurations and different scale problems are performed to compare the steepest descent method and the enhanced method. Finally, we give some conclusions and summarize our study.

2. Steepest Descent Method and Its Drawbacks

The steepest descent method is a line search technique which takes a step along the gradient direction a teach iteration. Let f(X) be the cost function, where X is the variable vector representing all variables in the mesh (the coordinates of free nodes). The steepest descent method modifies the vector at t-th iteration according to:

Δ X t = ε t X f ( X t ) (1)

where ΔXt is the change of the variable vector at t-th iteration, ÑX is the gradient operator with respect to the variable vector X, and εt is a small positive number called step length.

For global optimization-based smoothing, the dimension of the variable vector may be very big. For example, the dimension of the variable vector of a 2D mesh with 10,000 free nodes can be 20,000. The greater the dimension of the variable vector is, the more likely the gradient of the cost function will generate some special circumstances which will affect the convergence of the entire variable vector, such as the values in some dimensions of the gradient of the cost function are always close to 0, but in other dimensions of the gradient of the cost function are always lager. In this circumstance, the steepest descent is particularly slow. We show this case with a mesh in 2D consisting of 4 elements and 1 free node, as shown in Figure 1.

As shown in Figure 2, the cost function surface of the mesh seems like a narrow valley, the direction of the gradient is almost perpendicular to the long axis of the valley. The free node thus oscillates back and forth in the direction of the short axis, and moves very slowly along the long axis of the valley as shown in Figure 3.

Figure 1. The mesh with 4 elements and 1 free node.

Figure 2. The cost function surface of the mesh.

3. Enhanced Steepest Descent Method

In order to overcome the shortcomings of the steepest descent method, we present a variation of steepest descent method with the inclusion of a special term, as bellow:

Δ X t = ε t X f ( X t ) + p Δ X t 1 (2)

where p is the weight factor. The formula considers the change of the variable vector at the current time step with both the current gradient of the cost function and the weight change of the variable vector in previous step.

The rationale for use of the special term is that it can offset fluctuations in the direction of the short axis and speed up the movement in the direction of the long axis as shown in Figure 4.

The effect of the special term can also be illustrated with the addition of vectors. The special term tends to expend the current change of variable vector when the direction of current gradient of cost function is similar to that of the previous change, as shown in Figure 5(a), and tends to shorten the current change of variable vector when the direction of current gradient of cost function is different from that of the previous change, as shown in Figure 5(b).

Considering the momentum method:

Δ X t = ε t X f ( X t ) + p Δ X t 1 (3)

We can further obtain the relationship between ΔXt and ΔXtn by recursive, as bellow:

Δ X t = ε t X f ( X t ) p ε t 1 X f ( X t 1 ) + p 2 Δ X t 2 (4)

Δ X t = ε t X f ( X t ) p ε t 1 X f ( X t 1 ) p 2 ε t 2 X f ( X t 2 ) + p n Δ X t n (5)

Obviously, the larger p is, the more effect of ΔXtn on ΔXt is. when the directions

Figure 3. The node movement track of the steepest descent method.

Figure 4. The node movement track of the enhanced method.

(a) (b)

Figure 5. The effect of the momentum term. (a) The role of expending the current change; (b) The role of shortening the current change.

of ΔXti (i = 1, ..., n) are similar multiple times in succession, more accumulation of them is beneficial to the variable vector in current step converging to the optimal values at a faster speed. However, a larger p also means that it is difficult to stop when the variable vector reaches the optimal point. With extensive experiments, we found that it is effective to set the weight factor p to be 0.2.

4. Numerical Experiments

In this section, we will report results from a set of numerical experiments designed to compare the steepest descent method and the enhanced method. We consider triangular meshes and tetrahedral meshes separately.

Mesquite has implemented the steepest descent method already. We implement the enhanced method on the basis Mesquite. For step length ε, the Toolkit selects a big value and changes it to satisfy the Armijo condition [33]. When the Armijo condition is not met, the step length is reduced by a reduction factor; and when the step results in a tangled mesh, the step length is reduced by a back-tracking factor. We also employ the default parameter values in the enhanced method, where reduction factor is 0.5 and back-tracking factor is 0.2. Another important consideration in the study is the choice of cost function. We define the cost function as the sum of all element qualities according to the aspect ratio metric.

Aspect ratio quality metric is a commonly used quality metric in mesh smoothing. The quality value of an element with different configurations can vary significantly according to the metric. Various formulas have been used to compute the aspect ratio quality metric [3] [28]. We use a simple one implemented in Mesquite. For triangular element, it is defined as:

( l 1 2 + l 2 2 + l 3 2 ) / ( 4 3 × S ) (6)

And for tetrahedral element, it is defined as:

( l 1 2 + l 2 2 + l 3 2 + l 4 2 + l 5 2 + l 6 2 ) / ( 36 2 × V ) (7)

where li represents edge length, S represents area of triangular element, and V represents volume of tetrahedral element. The value of this metric range from 1 to ∞. The optimal value of the metric is 1.

Since the objective function used in our numerical experiments is non-convex, the different methods may converge to different local minimums. To ensure that this does not affect our experiments, we verified whether all methods converged to the same optimal mesh for each experiment by comparing the vertex coordinates of the optimal meshes. Unless otherwise stated, the methods converged to the same optimal mesh. In all experiments, the solution is considered optimal when it has converged to six significant digits.

4.1. Triangular Mesh Experiments

The triangular mesh examples are four Delaunay triangulations with different number of random points in the unit square as shown in Figures 6(a)-(d). Their uniformly distributed boundary nodes are fixed during the optimization process. The related results are listed in Table 1. It can be seen that the enhanced steepest descent method is far more efficient than the steepest descent method.

4.2. Tetrahedral Mesh Experiments

We chose three tetrahedral meshes with big scale problems and different initial configurations from mesquite example files as shown in Figures 7(a)-(c). Their boundary nodes are also fixed during the optimization process. The related results are listed in Table 2. It can also be seen that the enhanced steepest descent

(a) (b) (c) (d)

Figure 6. Four triangular meshes. (a) The first mesh with 398 elements; (b) The second mesh with 1198 elements; (c) The third mesh with 1598 elements; (d)The fourth mesh with 2198 elements.

Table 1. The performance of the two methods for triangular meshes.

(a) (b) (c)

Figure 7. Three tetrahedral meshes. (a) The first mesh with 112393 elements; (b) The second mesh with 23636 elements; (c) The third mesh with 11098 elements.

Table 2. The performance of the two methods for tetrahedral meshes.

method is more efficient than the steepest descent method.

5. Conclusions

In this paper, we presented an enhanced steepest descent method with same storage and almost negligible added computational cost as gradient descent method. Numerical experiments show that it can improve the speed of the mesh smoothing.

We presented a physically-based interpretation of the enhanced method. This give us insights explaining why it can work better than steepest descent method in global mesh smoothing.

Conflicts of Interest

The authors declare no conflicts of interest regarding the publication of this paper.

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