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Model Quality Report in Business Statistics - Harvard ...

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In the case of poststratification the auxiliary vector is def<strong>in</strong>ed by x = ( γ γ γ ) T<br />

k<br />

1 k<br />

,...,<br />

pk<br />

,...,<br />

Pk<br />

⎧1 if unit k ∈U<br />

p<br />

2<br />

where, for p = 1,..., P,<br />

γ<br />

pk<br />

= ⎨<br />

and σ k<br />

= 1 for all k. This poststratification<br />

⎩0<br />

otherwise<br />

approach gives us one simple method of deal<strong>in</strong>g with outly<strong>in</strong>g observations <strong>in</strong> a survey, s<strong>in</strong>ce<br />

they can be moved <strong>in</strong>to an appropriate poststratum for estimation.<br />

Most of the classical estimators can be derived as special cases from the GREG estimator.<br />

For example, if x<br />

k<br />

= xk<br />

for all k and σ 2 k<br />

∝ x k<br />

, where x k<br />

is a cont<strong>in</strong>uous variable, and when<br />

nonresponse model (i) is used, then the follow<strong>in</strong>g estimator is obta<strong>in</strong>ed:<br />

$t<br />

yr<br />

=<br />

H<br />

∑ N y<br />

h=<br />

1<br />

H<br />

h<br />

∑ N x<br />

h=<br />

1<br />

h<br />

rh<br />

rh<br />

∑<br />

U<br />

x<br />

k<br />

(2.13)<br />

Estimator (2.13) is sometimes called the comb<strong>in</strong>ed ratio estimator.<br />

Sometimes the group totals ∑U<br />

p<br />

x<br />

k<br />

are known and, <strong>in</strong> this general case, the p-groups are<br />

called model groups. Let us present a simple example. As before assume that x k<br />

is a<br />

cont<strong>in</strong>uous variable, but here we know the quantities ∑ ; p = 1,..., P. Let<br />

( γ x γ x γ x ) T<br />

x<br />

k<br />

=<br />

1 k k<br />

,...,<br />

pk k<br />

,...,<br />

Pk k<br />

, σ 2 k<br />

∝ x k<br />

for each p-group, and the RHGs co<strong>in</strong>cide with<br />

strata (nonresponse model (i)) then the GREG estimator takes the form<br />

U p<br />

x k<br />

t$<br />

yr<br />

=<br />

H<br />

$<br />

P<br />

∑ N<br />

h=<br />

1<br />

∑<br />

H<br />

p=<br />

1<br />

∑ N$<br />

h=<br />

1<br />

hp<br />

hp<br />

y<br />

x<br />

rhp<br />

rhp<br />

∑<br />

U p<br />

x<br />

k<br />

(2.14)<br />

If strata and model groups co<strong>in</strong>cide then estimator (2.14) can be written<br />

$t<br />

yr<br />

H yr<br />

h<br />

= ∑ ∑<br />

h=1<br />

x<br />

r<br />

h<br />

U<br />

h<br />

x<br />

k<br />

(2.15)<br />

Estimator (2.15) is sometimes called the separate ratio estimator.<br />

When x<br />

k<br />

= ( 1, xk<br />

) for all k and σ<br />

2 k<br />

= constant , then the classical regression estimator is<br />

obta<strong>in</strong>ed.<br />

Many bus<strong>in</strong>ess surveys are subject to occasional unusual observations, or outliers, which can<br />

have a large effect on the estimates. In these cases, robust versions of po<strong>in</strong>t estimators are<br />

often used, with the simplest be<strong>in</strong>g the poststratification estimator with the outliers <strong>in</strong> their<br />

own (completely enumerated) poststratum. This follows from the method above (2.13). Other<br />

methods <strong>in</strong>volve adjust<strong>in</strong>g the weights or the respond<strong>in</strong>g values, and w<strong>in</strong>sorisation is<br />

becom<strong>in</strong>g widely used with<strong>in</strong> the UK for treat<strong>in</strong>g outliers. This leads to a different estimator,<br />

which does not necessarily fit completely <strong>in</strong>to the GREG framework.<br />

8

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