The center-of-gravity method is a theoretic algorithm for convex optimization. It can be seen as a generalization of the bisection method from one-dimensional functions to multi-dimensional functions.[1]:{{{1}}} It is theoretically important as it attains the optimal convergence rate. However, it has little practical value as each step is very computationally expensive.
Our goal is to solve a convex optimization problem of the form:
minimize f(x) s.t. x in G,
where f is a convex function, and G is a convex subset of a Euclidean space Rn.
We assume that we have a "subgradient oracle": a routine that can compute a subgradient of f at any given point (if f is differentiable, then the only subgradient is the gradient [math]\displaystyle{ \nabla f }[/math]; but we do not assume that f is differentiable).
The method is iterative. At each iteration t, we keep a convex region Gt, which surely contains the desired minimum. Initially we have G0 = G. Then, each iteration t proceeds as follows.
Note that, by the above inequality, every minimum point of f must be in Gt+1.[1]:{{{1}}}
It can be proved that
[math]\displaystyle{ Volume(G_{t+1})\leq \left[1-\left(\frac{n}{n+1}\right)^n\right]\cdot Volume(G_t) }[/math] .
Therefore,
[math]\displaystyle{ f(x_t) - \min_G f \leq \left[1-\left(\frac{n}{n+1}\right)^n\right]^{t/n} [\max_G f - \min_G f] }[/math].
In other words, the method has linear convergence of the residual objective value, with convergence rate [math]\displaystyle{ \left[1-\left(\frac{n}{n+1}\right)^n\right]^{1/n} \leq (1-1/e)^{1/n} }[/math]. To get an ε-approximation to the objective value, the number of required steps is at most [math]\displaystyle{ 2.13 n \ln(1/\epsilon) + 1 }[/math].[1]:{{{1}}}
The main problem with the method is that, in each step, we have to compute the center-of-gravity of a polytope. All the methods known so far for this problem require a number of arithmetic operations that is exponential in the dimension n.[1]:{{{1}}} Therefore, the method is not useful in practice when there are 5 or more dimensions.
The ellipsoid method can be seen as a tractable approximation to the center-of-gravity method. Instead of maintaining the feasible polytope Gt, it maintains an ellipsoid that contains it. Computing the center-of-gravity of an ellipsoid is much easier than of a general polytope, and hence the ellipsoid method can usually be computed in polynomial time.
Original source: https://en.wikipedia.org/wiki/Center-of-gravity method.
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