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Stratified random sampling is a method used when parts of a population differ in the quantity being estimated. By separating the population into non-overlapping groups, or strata, and selecting a simple random sample from each, stratification can yield smaller error bounds, lower costs per observation, and stratum-specific estimates of population parameters. The process of drawing a stratified random sample, notation, and provides formulas for estimating population mean and total from stratified random sampling.
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Stratified Random Sampling When we know that parts of the population differ with respect to the quantity that we are estimating, we can obtain better estimates by using stratification. A stratified random sample is obtained by separating the population elements into nonoverlapping groups, called strata, and then se- lecting a simple random sample from each stratum. Stratification is particu- larly useful because: i) it can yield smaller error bounds than SRS, especially when the measurement is homogeneous within strata, ii) The cost per obser- vation can be lowered by appropriate choice of strata, and iii) it will yield stratum-specific estimates of population parameters. Drawing a Stratified Random Sample, notation: Choose strata, then take a SRS from each. L = number of strata, Ni = population size from stratum i, N = N 1 + N 2 + ... + NL = total population size, ni = sample size from stratum i, n = n 1 + n 2 + ... + nL = total sample size.
Estimation of a population mean and total from stratified ran- dom sampling: To estimate the mean μ from stratified random sampling, we use the sample stratified mean:
μ̂ = ¯yst =
[N 1 y¯ 1 + N 2 y¯ 2 + ... + NL y¯L] =
i=
Ni y¯i.
Since the strata are independent, we obtain the estimated variance by summing the estimated variances from each stratum:
Vˆ (¯yst) = 1 N 2
i=
N (^) i^2
Ni − ni Ni
s^2 i ni To estimate the total τ from stratified random sampling, we just estimate the total τi from each stratum and sum. Also, since the strata are indepen- dent, the estimated variance of the total is just the sum of the estimated variances from each stratum:
̂ τ =
i=
Ni y¯i and
Vˆ (̂τ ) =
i=
N (^) i^2
Ni − ni Ni
s^2 i ni