ST 380 Probability and Statistics for the Physical Sciences Parameter Estimation Probability theory tells us what to expect when we carry out some experiment with random outcomes, in terms of the parameters of the problem. Statistical theory tells us what we can learn about those parameters when we have seen the outcome of the experiment. We speak of making statistical inferences about the parameters. 1 / 16 Point Estimation Introduction
ST 380 Probability and Statistics for the Physical Sciences Point Estimation A point estimate of a parameter is a single value that represents a best guess as to the value of the parameter. For example, Rasmussen Reports surveyed 1,500 likely voters over a 3-day period, and 690 agreed that they approve the President’s performance in office. We assume that each voter was randomly selected from a population in which a fraction p of voters would agree. Here p is the parameter of interest, and the natural point estimate of it is ˆ p = 690 / 1500 = . 46, or 46%. 2 / 16 Point Estimation General Concepts
ST 380 Probability and Statistics for the Physical Sciences Sample Mean In any situation where we observe a simple random sample X 1 , X 2 , . . . , X n from some population with mean µ , we know that the sample mean ¯ X = ( X 1 + X 2 + · · · + X n ) / n satisfies E (¯ X ) = µ, so it is natural to estimate µ by ¯ X . We treat the Rasmussen survey as a binomial experiment with p (= ¯ E ( X i ) = p , so using ˆ X ) to estimate p is a special case of using ¯ X to estimate µ . 3 / 16 Point Estimation General Concepts
ST 380 Probability and Statistics for the Physical Sciences Estimator and Estimate It is important to distinguish between the rule that we follow to estimate a parameter and the value that we find for a particular sample. We call the rule an estimator and the value an estimate . For example, in the survey data, the rule is “estimate p by the sample fraction ˆ p ”, and the value is .46. So the estimator is ˆ p , and the estimate is .46. One week ago, the same estimator ˆ p with a different sample gave a different estimate , .49. 4 / 16 Point Estimation General Concepts
ST 380 Probability and Statistics for the Physical Sciences Sampling Distribution Clearly a point estimator is a statistic, and therefore has a sampling distribution. Suppose that X 1 , X 2 , . . . , X n is a random sample from some population with a parameter θ , and that θ = ˆ ˆ θ ( X 1 , X 2 , . . . , X n ) is a statistic that we want to use as an estimator of θ . 5 / 16 Point Estimation General Concepts
ST 380 Probability and Statistics for the Physical Sciences Bias If E (ˆ θ ) = θ for all possible values of θ , ˆ θ is an unbiased estimator of θ . In general, the bias of ˆ θ as an estimator of θ is E (ˆ θ − θ ) = E (ˆ θ ) − θ. A biased estimator in a sense systematically over-estimates or under-estimates θ , so we try to avoid estimators with large biases. An unbiased estimator is desirable, but not always available, and not always sensible. 6 / 16 Point Estimation General Concepts
ST 380 Probability and Statistics for the Physical Sciences For example, suppose that n = 1, and X = X 1 has the Poisson distribution with parameter µ : P ( X = x ) = p ( x ; µ ) = e − µ µ x x ! , x = 0 , 1 , . . . E ( X ) = µ , so X is an unbiased estimator of µ , but suppose that the parameter of interest is θ = e − µ . The only unbiased estimator of θ is � 1 if X = 0 , ˆ θ = 0 if X > 0 . 7 / 16 Point Estimation General Concepts
ST 380 Probability and Statistics for the Physical Sciences Mean Squared Error We measure how far an estimator ˆ θ is from the true value θ using the mean squared error : MSE(ˆ θ ; θ ) = E [(ˆ θ − θ ) 2 ] . We can show that θ ; θ ) = (bias) 2 + V (ˆ MSE(ˆ θ ) . For an unbiased estimator, bias = 0, so MSE(ˆ θ ; θ ) = V (ˆ θ ) . 8 / 16 Point Estimation General Concepts
ST 380 Probability and Statistics for the Physical Sciences Many biased estimators are approximately unbiased, in the sense that (bias) 2 ≪ V (ˆ θ ) , so MSE(ˆ θ ; θ ) ≈ V (ˆ θ ) . Standard error So if an estimator is unbiased, either exactly or approximately, its performance is measured by V (ˆ θ ), or by its standard deviation � V (ˆ σ ˆ θ = θ ) , also known as its standard error . 9 / 16 Point Estimation General Concepts
ST 380 Probability and Statistics for the Physical Sciences Often an estimator’s standard error is a function of θ or other parameters; these must be replaced by estimates before we can actually calculate a value. Estimated standard error The resulting statistic is called the estimated standard error, and is denoted ˆ σ ˆ θ . Example: binomial distribution; V (ˆ p ) = p (1 − p ) / n , so � � p (1 − p ) p (1 − ˆ ˆ p ) σ ˆ p = , and ˆ σ ˆ p = . n n 10 / 16 Point Estimation General Concepts
ST 380 Probability and Statistics for the Physical Sciences Methods of Point Estimation In some situations we have an obvious estimator ˆ θ , such as the binomial ˆ p = X / n . In other cases we may not. Example: Ozone pollution Suppose that X 1 , X 2 , . . . , X 28 are daily maximum ozone levels on 28 consecutive days. Suppose further that we want to model these as independent variables with the Weibull distribution � α − 1 f ( x ; α, β ) = α � x e − ( x /β ) α , 0 < x < ∞ . β β 11 / 16 Point Estimation Methods of Point Estimation
ST 380 Probability and Statistics for the Physical Sciences It is not obvious how to estimate either α or β . Suppose that we know from other data that α is well approximated by the value 2. It is still not obvious how to estimate β . Before we observed the data, the joint pdf n � f ( x i ; α, β ) i =1 measures the relative probability of observing specific values x 1 , x 2 , . . . , x n . 12 / 16 Point Estimation Methods of Point Estimation
ST 380 Probability and Statistics for the Physical Sciences Likelihood function After observing x 1 , x 2 , . . . , x n , we can use the same function to measure the relative likelihood of different values of α and β (or just β if we believe we know the value of α = α 0 ). When used this way, we call it the likelihood function , n � L ( β ) = f ( x i ; α 0 , β ) . i =1 13 / 16 Point Estimation Methods of Point Estimation
ST 380 Probability and Statistics for the Physical Sciences Example, with simulated ozone levels: n <- 28 alpha0 <- 2 beta <- 70 x <- rweibull(n, alpha0, beta) L <- function(beta) { lik <- rep(NA, length(beta)) for (i in 1:length(beta)) lik[i] <- prod(dweibull(x, alpha0, beta[i])) lik } plot(L, from = 50, to = 100) 14 / 16 Point Estimation Methods of Point Estimation
ST 380 Probability and Statistics for the Physical Sciences Maximum Likelihood The most likely value of β , the value that maximizes the likelihood, is the maximum likelihood estimate. Maximum likelihood estimators are generally approximately unbiased, and have close to the smallest possible mean squared error. Most of the estimators that we cover later will be maximum likelihood estimators, or sometimes unbiased modifications of them. 15 / 16 Point Estimation Methods of Point Estimation
ST 380 Probability and Statistics for the Physical Sciences In the example, we can use the optimize() function to find the maximum likelihood estimate of β : o <- optimize(L, c(50, 100), maximum = TRUE) abline(v = o$maximum, col = "blue") title(paste("MLE of beta:", round(o$maximum, 1))) Alternatively, we can show analytically that �� x α 0 � 1 α 0 ˆ i β ML = n mean(x^alpha0)^(1/alpha0) 16 / 16 Point Estimation Methods of Point Estimation
Recommend
More recommend
