UNIVERSITY OF COLORADO AT DENVER
PLACE: Mathematics Conference Room 626 UCD Building, 1250 14th St., Denver
TIME: noon (Refreshments served at 11:45 am)
DATE: February 1, 1999
SPEAKER: Ben Fox
TITLE: Quasi-Monte Carlo for PDEs
ABSTRACT:
Like ordinary standard Monte Carlo (MC),
quasi-Monte Carlo (QMC) estimates an integral
by averaging the integrand at certain points.
The latter, however, uses points that are
"better spaced". In traditional QMC, these
are selected deterministically.
Perhaps contrary to intuition,
in more than one dimension, grids are not
"well spaced". We take the domain of the integral
as the unit cube, if necessary mapping invertibly
from another domain.
How does this connect to PDEs ?
An obvious good case for MC or QMC occurs when we want
the solution only at a few selected points.
More generally, we may want to estimate functionals of
the solution.
For example, the integral can be an L_p-norm of the
solution or of the "error".
In the latter case, the error can be measured relative
deviations from
a known solution (for checking a more general code)
or from an estimated solution (to assess its "reliability").
For stochastic PDEs (with noisy coefficents and/or
right side generated by a random field), the integral
can be the expectation of the error. For each input
realization of the field, a deterministic PDE-solver
(or, for the cases above, QMC)
produces an estimated solution. Average these estimates
to get the overall estimate.
In the talk, I deal with the Gaussian case.
Amazing to me (but not due to me),
the pointwise solution to
both generalized heat equations
of a certain form and Poisson's equation with enough
smoothness can be recast in terms of Brownian motion.
For stochastic PDEs, I take the random field to
be Gaussian.
I show how to structure the simulation to increase
efficiency of QMC. A "randomized" version of QMC
will be indicated. This gives a way to estimate error,
via iid copies of QMC "blocks",
and also takes greater advantage of smoothness,
increasing simulation efficiency by another order
of magnitude.