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Monte Carlo Methods in Statistical Mechanics: Foundations and ...

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unfeasible, but we are free to useany updat<strong>in</strong>g that leaves <strong>in</strong>variant the appropriate<br />

conditional distributions. Of course, <strong>in</strong> this generality \partial resampl<strong>in</strong>g" <strong>in</strong>cludes all<br />

dynamic <strong>Monte</strong> <strong>Carlo</strong> algorithms | we could just take f g to bethe entire system<br />

|butitis<strong>in</strong>many cases conceptually useful to focus on some subset of variables.<br />

The partial-resampl<strong>in</strong>g idea will be at the heart of the multi-grid <strong>Monte</strong> <strong>Carlo</strong> method<br />

(Section 5) <strong>and</strong> the embedd<strong>in</strong>g algorithms (Section 6).<br />

We have nowde nedarather large class of dynamic <strong>Monte</strong> <strong>Carlo</strong> algorithms: the<br />

s<strong>in</strong>gle-sp<strong>in</strong>- ip Metropolis algorithm, the s<strong>in</strong>gle-site heat-bath algorithm, <strong>and</strong> so on.<br />

How well do these algorithms perform? Away from phase transitions, they perform<br />

rather well. However, nearaphase transition, the autocorrelation time grows rapidly.<br />

In particular, near a critical po<strong>in</strong>t (second-order phase transition), the autocorrelation<br />

time typically diverges as<br />

m<strong>in</strong>(L ) z (4.20)<br />

where L is the l<strong>in</strong>ear size of the system, is the correlation length ofan<strong>in</strong> nite-volume<br />

system atthe sametemperature, <strong>and</strong> z is a dynamic critical exponent. This phenomenon<br />

is called critical slow<strong>in</strong>g-down itseverely hampers the study of critical phenomena by<br />

<strong>Monte</strong> <strong>Carlo</strong> methods. Most of therema<strong>in</strong>der of these lectures will be devoted, therefore,<br />

to describ<strong>in</strong>g recent progress <strong>in</strong> <strong>in</strong>vent<strong>in</strong>g new <strong>Monte</strong> <strong>Carlo</strong> algorithms with radically<br />

reduced critical slow<strong>in</strong>g-down.<br />

The critical slow<strong>in</strong>g-down of the conventional algorithms arises fundamentally from<br />

the factthat their updates are local: <strong>in</strong>as<strong>in</strong>gle step of the algorithm, \<strong>in</strong>formation" is<br />

transmitted from a given siteonlytoitsnearest neighbors. Crudely onemightguessthat<br />

this \<strong>in</strong>formation" executes a r<strong>and</strong>om walk around thelattice. In order for the system to<br />

evolve to an \essentially new" con guration, the \<strong>in</strong>formation" has to travel a distance<br />

of order ,the (static) correlation length. One would guess, therefore, that 2 near<br />

criticality, i.e. that the dynamic critical exponent z equals 2. This guess is correct for<br />

the Gaussian model (free eld). 12 For other models, we have asituation analogous to<br />

theory of static critical phenomena: thedynamic critical exponentisanontrivial number<br />

that characterizes a rather large class of algorithms (a so-called \dynamic universality<br />

class"). In any case, for most models of <strong>in</strong>terest, the dynamic critical exponent for<br />

local algorithms is close to 2(usuallysomewhat higher) [21]. Accurate measurements<br />

of dynamic critical exponents are,however, very di cult |even more di cult than<br />

measurements ofstatic critical exponents |<strong>and</strong> require enormous quantities of <strong>Monte</strong><br />

<strong>Carlo</strong> data: run lengths of 10000 ,when is itself gett<strong>in</strong>g large!<br />

We can now make a rough estimate ofthe computer time needed to study the Is<strong>in</strong>g<br />

model near its critical po<strong>in</strong>t, or quantum chromodynamics near the cont<strong>in</strong>uum limit.<br />

Eachsweepofthelattice takes a timeoforder L d ,where d is thespatial (or space-\time")<br />

dimensionality ofthe model. And weneed 2 sweeps <strong>in</strong> order to get one \e ectively<br />

12 Indeed, for the Gaussian model this r<strong>and</strong>om-walk picture can be made rigorous: see [19] comb<strong>in</strong>ed<br />

with [20, Section 8].<br />

21

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