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Extreme Value Analysis
FISH 558 Decision Analysis in Natural Resource Management 11/30/2015 Noble Hendrix QEDA Consulting LLC Affiliate Faculty UW SAFS
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Lecture Overview Motivating examples of extreme events
Generalized Extreme Value Statistical Development Case Study: the white cliffs of Dover Generalized Pareto Distribution Case Study: whale strikes in SE Alaska Additional resources
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Why should we care about extreme events?
They are rare by definition, so why spend much time thinking about them? Often the consequences of the event have significant impacts to the system – mortality, colonization, episodic recruitment We tend to focus on averages, but extremes may be more important in some situations. We may also be interested in estimating extremes beyond what has been observed
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Distribution of outcomes
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Distribution of outcomes
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Distribution of outcomes
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Distribution of outcomes
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Distribution of outcomes
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Motivation 100 year floodplain
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Motivation Surpassing the 100 year floodplain
Road and home construction based on flood frequency and intensity i.e., 100 year floodplain
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Motivation Hurricanes
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Financial Markets
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Statistical Foundations
Central Limit Theorem Consider sequence of iid random variables, X1, … Xn We know that sum Sn = X1 + … + Xn, when normalized lead to the CLT: Statistical Foundations
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Generalized Extreme Value Fisher-Tippet Asymptotic Theorem
Define maxima of sequence of random variables Mn = max(X1, …, Xn) For normalized maxima, there is also a non-degenerate distribution H(x), which is a GEV distribution
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Generalized Extreme Value Cumulative Density Function
u – location s – scale v - shape
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Generalized Extreme Value Variants of the GEV
Shape parameter v defines several distributions: Gumbel: v = 0 Weibull: v < 0 Fréchet: v > 0
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Generalized Extreme Value Shapes of GEV
Weibull Gumbel Fréchet
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Generalized Extreme Value Applicability
Almost all common continuous distributions converge on H(x) for some value of v Weibull – beta Gumbel – normal, lognormal, hyperbolic, gamma, chi-squared Fréchet – Pareto, inverse gamma, Student t, loggamma
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Generalized Extreme Value Minima
What about minima? min(X1, …, Xn) = - max(-X1, … ,-Xn) If H(x) is the limiting distribution for maxima, then 1 – H(-x) is the limiting distribution for minima, so can also be handled
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Generalized Extreme Value Estimation
Obtain data from an unknown distribution F Let’s assume that there is an extreme value distribution Hv for some value of v The true distribution of the n-block maximum Mn can be approximated for large enough n with a GEV distribution H(x) Fit model to repeated observations of an n-block maximum, thus m blocks of size n
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Generalized Extreme Value Example - Data
Annual sea level height at Dover, Britain between 1912 and 1992
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Generalized Extreme Value Example - Data
Annual sea level height at Dover, Britain between 1912 and 1992
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Generalized Extreme Value R package evd
> require(evd) > data(sealevel) > sl.no<-na.omit(sealevel[,1]) > fgev(sl.no) Call: fgev(x = sl.no) Deviance: Estimates loc scale shape Standard Errors loc scale shape
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Generalized Extreme Value Diagnostics
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Generalized Extreme Value Return Level Plot
Return level – “how long to wait on average until see another event equal to or more extreme” If H is the distribution of the n-block maximum, the k return level is the 1 – 1/k quantile of H
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Generalized Extreme Value Profile likelihood of parameters
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Generalized Extreme Value Limitations
Limitations of the GEV: Used for block maxima, e.g., annual precipitation, annual flow, Only 1 exceedance per block May ignore some important observations, Some go so far as to say it is a wasteful method! (McNeil et al Quantitative Risk Management, Princeton)
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Generalized Pareto Distribution
GEV has largely been surpassed by another method for extremes over a threshold Pickands (1975) developed a model for excesses y over threshold a Pickands 1975 Annals of Stats 3:119
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Generalized Pareto Distribution
a – threshold b – scale v - shape
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Generalized Pareto Distribution Shapes of GPD
Positive shape = limitless loss
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Generalized Pareto Distribution Applicability
For any continuous distributions that converge on H(x) for some value of v, which was most of the continuous distributions of interest The same distributions will converge on G(x) as an excess distribution as the threshold a is raised
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Generalized Pareto Distribution Estimation
Obtain data from an unknown distribution F Calculate Yj = Xj – a for Na that exceed threshold a maximize log-likelihood:
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Generalized Pareto Distribution Threshold Estimation
Have an interesting problem: Need a value of threshold a that must be high enough to satisfy the theoretical assumptions Need enough data above the threshold a so that the parameters are well estimated Use a sample mean residual life plot to help identify a reasonable threshold value a
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Generalized Pareto Distribution Sample Mean Residual Life Plot
Let Y = X – a0. At threshold a0, if Y is GPD with parameters b and v then E(Y) = b/(1 – v), v < 1 This is true for all thresholds ai > a0, but the scale parameter bi must be appropriate to the threshold ai E(X-ai| X > ai) = (bi + v*ai)/(1-v), Thus E(X - a| X > a) is a linear function of a where GPD appropriate, so can plot E(x-ai) (where x are our observed data) versus ai. This is the sample mean residual life plot, and confidence intervals added by assuming E(x-a) are approximately normally distributed
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Generalized Pareto Distribution Example - Data
Quantifying strike rates of whales in southeast Alaska
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Generalized Pareto Distribution Distances to Whales
Minimum distances (i.e., D < 0) are where losses occur, so transform distance D into a positive loss metric, where value of 100 equates to D = 0
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Generalized Pareto Distribution Whale Distance Metric
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Generalized Pareto Distribution Threshold determination
Looking for discontinuities in the mean excess, E(x-ai), at different threshold values ai Identified value of 70 as the threshold (equates to a distance of 300m between whales and ships)
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Generalized Pareto Distribution Threshold determination
library(POT) mrlplot(w.metric, xlim = c(50,90) ) tcplot(w.metric, u.range = c(50, 90) ) Mean residual life plot (previous slide) indicates a = 70 Discontinuity in scale and shape estimates when threshold a > 70
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Generalized Pareto Distribution Estimation
> fitgpd(w.metric, thresh = 70, est = "mle") Estimator: MLE Deviance: AIC: Varying Threshold: FALSE Threshold Call: 70 Number Above: 151 Proportion Above: Estimates scale shape Standard Error Type: observed Standard Errors scale shape Asymptotic Variance Covariance scale shape scale shape Optimization Information Convergence: successful
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Generalized Pareto Distribution Diagnostics
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Generalized Pareto Distribution Likelihood profiles
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Generalized Pareto Distribution Likelihood profiles with different thresholds
relative log likelihood - likelihood relative to maximum for that threshold value
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Generalized Pareto Distribution Empirical and Estimated
Comparison of empirical (no observed strikes) and GPD model estimates for a = 70 Since 2000, 2 confirmed strikes GPD provides better characterization of risk Empirical GPD
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Generalized Pareto Distribution Return Level
Return level – how many encounters where whales are less than 300m until a strike? Conditional return level of approx. 500 Absolute return level of approx (1 in 5 encounters has an encounter < 300m)
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Summary: GEV and EVT Generalized Extreme Value (GEV) distribution
Used for block maxima, e.g., maximum sea-level per year Data loss due to only block maxima Generalized Pareto Distribution (GPD) Used for points over a threshold All exceedances above some limit are used Question about how to deal with selecting a threshold value
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Additional Resources Books and Papers
Coles, S An Introduction to Statistical Modelling of Extreme Values. Springer Series in Statistics. London. McNeil, A. J., Frey, R., & Embrechts, P Quantitative risk management: concepts, techniques, and tools. Princeton University Press. Embrechts, P Modelling extremal events: for insurance and finance (Vol. 33). Springer. Bayesian GPD Modeling Coles, S. and L. Pericchi Anticipating catastrophes through extreme value modeling. Applied Statistics 52(4): 405–416. Jagger. T. H. and J. B. Elsne Climatology models for extreme hurricane winds near the United States. Journal of Climate 19:
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Additional Resources Fitting models in R and BUGS
A few R packages Points over Threshold (POT) Extreme Value Distributions (evd) extRemes Quantitative Risk Management (QRM) evdbayes BUGS OpenBUGS – GEV and GPD WinBUGS/JAGS – GPD with 1’s trick
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