Optimisation

Resources:

First-order Methods

Momentum: Instead of just using past gradient, create a weighted average of all the past gradients.

  • , where is the momentum and is the gradient of the objective function at step t, and .
  • Why does using past gradients reach convergence faster?

  • Problem with simple momentum is that it not slow down enough at the bottom of the valley.

Nesterov Momentum:

  • For each step, Nesterov’s momentum uses gradient at new location instead of current location.

Second order Methods

Newton’s method: , where .

  • when Hessian is convex, the descent direction is chosen as
  • Can be derived using taylor approximation of around , and finding the minimum.
  • BFGS
  • Trust region: Do the opposite of line search, i.e. instead of determining the direction and then travelling optimally. Determine the distance first, and then solve for optimal direction.
    • around parameter determine a Region , where objective function can be approximated as locally as a quadratic using taylor approximation.
    • At each step, we solve: , where .
    • If is taken as a ball of radius r, then adding a Lagrange multiplier to M, .
    • Solve this using , i.e. can be taken such that all eigenvalues are non-negative, and convex optimization methods like Momentum can be applied.

SGD

Lagrange Multipliers: Calculus III - Lagrange Multipliers

Steepest Descent: Done using different norms: Lp norms.

derive dual norm of subject to arbitrary norm .

Dual formulation of steepest descent

  • From the definition of dual norm, which implies, for any unit vector ,
  • Flipping the sign and adding the extra term:
  • Our goal is to find to minimise . Let , taking the gradient, we get .
  • Now, from dual norm, . This becomes an equality when .
  • Thus

For based norm, dual norm = standard norm and , then . This is the standard Gradient descent formula.

For based norm, dual norm = norm and , then . Note that, this is equivalent to Adam update when setting the parameters . So, direction depends only on the sign and not the magnitude.

EM