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Lecture 2: Parameter Estimation and Evaluation of Support

Likelihood Methods in Ecology April 25 - 29, 2011 Granada, Spain. Lecture 2: Parameter Estimation and Evaluation of Support. Parameter Estimation.

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Lecture 2: Parameter Estimation and Evaluation of Support

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  1. Likelihood Methods in Ecology April 25 - 29, 2011 Granada, Spain Lecture 2:Parameter Estimation and Evaluation of Support

  2. Parameter Estimation “The problem of estimation is of more central importance, (than hypothesis testing)..for in almost all situations we know that the effect whose significance we are measuring is perfectly real, however small; what is at issue is its magnitude.” (Edwards, 1992, pg. 2) “An insignificant result, far from telling us that the effect is non-existent, merely warns us that the sample was not large enough to reveal it.” (Edwards, 1992, pg. 2)

  3. Parameter Estimation • Finding Maximum Likelihood Estimates (MLEs) • Local optimization (optim) • Gradient methods • Simplex (Nelder-Mead) • Global optimization • Simulated Annealing (anneal) • Genetic Algorithms (rgenoud) • Evaluating the strength of evidence (“support”) for different parameter estimates • Support Intervals • Asymptotic Support Intervals • Simultaneous Support Intervals • The shape of likelihood surfaces around MLEs

  4. Parameter estimation: finding peaks on likelihood “surfaces”... The variation in likelihood for any given set of parameter values defines a likelihood “surface”... The goal of parameter estimation is to find the peak of the likelihood surface.... (optimization)

  5. Local vs Global Optimization • “Fast” local optimization methods • Large family of methods, widely used for nonlinear regression in commercial software packages • “Brute force” global optimization methods • Grid search • Genetic algorithms • Simulated annealing global optimum local optimum

  6. Local Optimization – Gradient Methods • Derivative-based (Newton-Raphson) methods: Likelihood surface General approach: Vary parameter estimate systematically and search for zero slope in the first derivative of the likelihood function...(using numerical methods to estimate the derivative, and checking the second derivative to make sure it is a maximum, not a minimum)

  7. Local Optimization – No Gradient • The Simplex (Nelder Mead) method • Much simpler to program • Does not require calculation or estimation of a derivative • No general theoretical proof that it works, (but lots of happy practitioners…)

  8. Global Optimization “Virtually nothing is known about finding global extrema in general.” “There are tantalizing hints that so-called “annealing methods” may lead to important progress on global (optimization)...” Quote from Press et al. (1986) Numerical Recipes

  9. Global Optimization – Grid Searches • Simplest form of optimization (and rarely used in practice) • Systematically search parameter space at a grid of points • Can be useful for visualization of the broad features of a likelihood surface

  10. Global Optimization – Genetic Algorithms • Based on a fairly literal analogy with evolution • Start with a reasonably large “population” of parameter sets • Calculate the “fitness” (likelihood) of each individual set of parameters • Create the next generation of parameter sets based on the fitness of the “parents”, and various rules for recombination of subsets of parameters (genes) • Let the population evolve until fitness reaches a maximum asymptote

  11. Global optimization - Simulated Annealing • Analogy with the physical process of annealing: • Start the process at a high “temperature” • Gradually reduce the temperature according to an annealing schedule • Always accept uphill moves (i.e. an increase in likelihood) • Accept downhill moves according to the Metropolis algorithm: p = probability of accepting downhill move Dlh = magnitude of change in likelihood t = temperature

  12. Effect of temperature (t)

  13. Simulated Annealing in practice... A version with automatic adjustment of range... Search range (step size) Lower bound Upper bound Current value REFERENCES: Goffe, W. L., G. D. Ferrier, and J. Rogers. 1994. Global optimization of statistical functions with simulated annealing. Journal of Econometrics 60:65-99. Corana et al. 1987. Minimizing multimodal functions of continuous variables with the simulated annealing algorithm. ACM Transactions on Mathematical Software 13:262-280

  14. Constraints – setting limits for the search... • Biological limits • Values that make no sense biologically (be careful...) • Algebraic limits • Values for which the model is undefined (i.e. dividing by zero...) Bottom line: global optimization methods let you cast your net widely, at the cost of computer time...

  15. Simulated Annealing - Initialization • Set • Annealing schedule • Initial temperature (t) (3.0) • Rate of reduction in temperature (rt) (0.95)N • Interval between drops in temperature (nt) (100) • Interval between changes in range (ns) (20) • Parameter values • Initial values (x) • Upper and lower bounds (lb,ub) • Initial range (vm) Typical values in blue...

  16. Simulated Annealing – Step 1 Pick a new set of parameter values (by varying just 1 parameter) Begin {a single iteration} {copy the current parameter array (x) to a temporary holder (xp) for this iteration} xp := x; {choose a new value for the parameter in use (puse)} xp[puse] := x[puse] + ((random*2 - 1)*vm[puse]); {check if the new value is out of bounds } if xp[puse] < lb[puse] then xp[puse] := x[puse] - (random * (x[puse]-lb[puse])); if xp[puse] > ub[puse] then xp[puse] := x[puse] + (random * (ub[puse]-x[puse])); vm is the range lb is the lower bound ub is the upper bound

  17. Simulated Annealing – Step 2 {call the likelihood function with the new set of parameter values} likeli(xp,fp); {fp = new likelihood} {accept the new values if likelihood increases or at least stays the same} if (fp >= f) then begin x := xp; f := fp; nacp[puse] := nacp[puse] + 1; if (fp > fopt) then {if this is a new maximum, update the maximum likelihood} begin xopt := xp; fopt := fp; opteval := eval; BestFit; {update display of maximum r} end; end Accept the step if it leads uphill...

  18. Simulated Annealing – Step 3 else{use Metropolis criteria to determine whether to accept a downhill move } begin try {fp < f, so the code below is a shortcut for exp(-1.0(abs(f-fp)/t)} p := exp((fp-f)/t); {t = current temperature} except on EUnderflow do p := 0; end; pp := random; if pp < p then begin x := xp; f := fp; nacp[puse] := nacp[puse] + 1; end; end; Use the Metropolis algorithm to decide whether to accept a downhill step...

  19. Simulated Annealing – Step 4 Periodically adjust the range (VM) within which new steps are chosen... {after nused * ns cycles, adjust VM so that half of evaluations are accepted} If eval mod (nused*ns) = 0 then begin for i := 0 to npmax do if xvary[i] then begin ratio := nacp[i]/ns; { C controls the adjustment of VM (range) - references suggest setting at 2.0} if (ratio > 0.6) then vm[i] := vm[i]*(1.0+c[i]*((ratio - 0.6)/0.4)) else if ratio < 0.4 then vm[i] := vm[i]/(1.0+c[i]*((0.4 - ratio)/0.4)); if vm[i] > (ub[i]-lb[i]) then vm[i] := ub[i] - lb[i]; end; { reset nacp[i]} for i := 1 to npmax do nacp[i] := 0; end; ns is typically ~ 20 This part is strictly ad hoc...

  20. Effect of C on Adjusting Range...

  21. Simulated Annealing Code – Final Step Reduce the “temperature” according to the annealing schedule {after nused * ns * nt cycles, reduce temperature t } If eval mod (nused*ns*nt) = 0 then begin t := rt * t; {store current maximum lhood in history list} lhist[eval div (nused*ns*nt)].iter := eval; lhist[eval div (nused*ns*nt)].lhood := fopt; end; I typically set nt = 100 (a very slow annealing) rt = fractional reduction in temperature at each drop in temperature: NOTE: Goffe et al. restart the search at the previous MLE estimates each time the temperature drops... (I don’t)

  22. How many iterations?... Logistic regression of windthrow susceptibility (188 parameters) 5 million is not enough! Red maple leaf litterfall (6 parameters) 500,000 is way more than necessary! What would constitute convergence?...

  23. Optimization - Summary • No hard and fast rules for any optimization – be willing to explore alternate options. • Be wary of initial values used in local optimization when the model is at all complicated • How about a hybrid approach? Start with simulated annealing, then switch to a local optimization…

  24. Evaluating the strength of evidence for the MLE Now that you have an MLE, how should you evaluate it? (Hint: think about the shape of the likelihood function, not just the MLE)

  25. Strength of evidence for particular parameter estimates – “Support” Log-likelihood = “Support” (Edwards 1992) • Likelihood provides an objective measure of the strength of evidence for different parameter estimates...

  26. Fisher’s “Score” and “Information” • “Score” (a function) = First derivative (slope) of the likelihood function • So, S(θ) = 0 at the maximum likelihood estimate of θ • “Information” (a number) = -1 * Second derivative (acceleration) of the likelihood function, evaluated at the MLE.. • So this is a number: a measure of how steeply likelihood drops off as you move away from the MLE • In general cases, “information” is equivalent to the variance of the parameter…

  27. Parameter 2 Parameter 1 Profile Likelihood • Evaluate support (information) for a range of values of a given parameter by treating all other parameters as “nuisance” and holding them at their MLEs…

  28. Asymptotic vs. Simultaneous M-Unit Support Limits • Asymptotic Support Limits (based on Profile Likelihood): • Hold all other parameters at their MLE values, and systematically vary the remaining parameter until likelihood declines by a chosen amount (m)... What should “m” be? (2 is a good number, and is roughly analogous to a 95% CI)

  29. Asymptotic vs. Simultaneous M-Unit Support Limits • Simultaneous: • Resampling method: draw a very large number of random sets of parameters and calculate log-likelihood. M-unit simultaneous support limits for parameter xi are the upper and lower limits that don’t differ by more than m units of support... In practice, it can require an enormous number of iterations to do this if there are more than a few parameters

  30. Asymptotic vs. Simultaneous Support Limits A hypothetical likelihood surface for 2 parameters... Simultaneous 2-unit support limits for P1 2-unit drop in support Parameter 2 Asymptotic 2-unit support limits for P1 Parameter 1

  31. Other measures of strength of evidence for different parameter estimates • Edwards (1992; Chapter 5) • Various measures of the “shape” of the likelihood surface in the vicinity of the MLE... How pointed is the peak?...

  32. Bootstrap methods • Bootstrap methods can be used to estimate the variances of parameter estimates • In simple terms: • generate many replicates of the dataset by sampling with replacement (bootstraps) • Estimate parameters for each of the datasets • Use the variance of the parameter estimates as a bootstrap estimate of the variance

  33. Evaluating Support for Parameter Estimates: A Frequentist Approach • Traditional confidence intervals and standard errors of the parameter estimates can be generated from the Hessian matrix • Hessian = matrix of second partial derivatives of the likelihood function with respect to parameters, evaluated at the maximum likelihood estimates • Also called the “Information Matrix” by Fisher • Provides a measure of the steepness of the likelihood surface in the region of the optimum • Can be generated in R using optim and fdHess

  34. Example from R The Hessian matrix (when maximizing a log likelihood) is a numerical approximation for Fisher's Information Matrix (i.e. the matrix of second partial derivatives of the likelihood function), evaluated at the point of the maximum likelihood estimates. Thus, it's a measure of the steepness of thedrop in the likelihood surface as you move away from the MLE. > res$hessian a b sd a -150.182 -2758.360 -0.201 b -2758.360 -67984.416 -5.925 sd -0.202 -5.926 -299.422 (sample output from an analysis that estimates two parameters and a variance term)

  35. More from R now invert the negative of the Hessian matrix to get the matrix of parameter variance and covariance > solve(-1*res$hessian) a b sd a 2.613229e-02 -1.060277e-03 3.370998e-06 b -1.060277e-03 5.772835e-05 -4.278866e-07 sd 3.370998e-06 -4.278866e-07 3.339775e-03 the square roots of the diagonals of the inverted negative Hessian are the standard errors* > sqrt(diag(solve(-1*res$hessian))) a b sd 0.1616 0.007597 0.05779 (*and 1.96 * S.E. is a 95% C.I….)

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