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Econometric Analysis of Cross Section and Panel Data - Free

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Discrete Response Models 473<br />

The model is applicable when y 2 is correlated with u 1 because <strong>of</strong> omitted variables<br />

or measurement error. It can also be applied to the case where y 2 is determined jointly<br />

with y 1 , but with a caveat. If y 1 appears on the right-h<strong>and</strong> side in a linear structural<br />

equation for y 2 , then the reduced form for y 2 cannot be found with v 2 having the<br />

stated properties. However, if y 1 appears in a linear structural equation for y 2, then<br />

y 2 has the reduced form given by equation (15.40); see Maddala (1983, Chapter 7)<br />

for further discussion.<br />

The normalization that gives the parameters in equation (15.39) an average partial<br />

e¤ect interpretation, at least in the omitted variable <strong>and</strong> simultaneity contexts, is<br />

Varðu 1 Þ¼1, just as in a probit model with all explanatory variables exogenous. To<br />

see this point, consider the outcome on y 1 at two di¤erent outcomes <strong>of</strong> y 2 , say y 2 <strong>and</strong><br />

y 2 þ 1. Holding the observed exogenous factors fixed at z 1 , <strong>and</strong> holding u 1 fixed, the<br />

di¤erence in responses is<br />

1½z 1 d 1 þ a 1 ðy 2 þ 1Þþu 1 b 0Š<br />

1½z 1 d 1 þ a 1 y 2 þ u 1 b 0Š<br />

(This di¤erence can take on the values 1, 0, <strong>and</strong> 1.) Because u 1 is unobserved, we<br />

cannot estimate the di¤erence in responses for a given population unit. Nevertheless,<br />

if we average across the distribution <strong>of</strong> u 1 , which is Normalð0; 1Þ, we obtain<br />

F½z 1 d 1 þ a 1 ðy 2 þ 1ÞŠ<br />

Fðz 1 d 1 þ a 1 y 2 Þ<br />

Therefore, d 1 <strong>and</strong> a 1 are the parameters appearing in the APE. [Alternatively, if we<br />

begin by allowing s1 2 ¼ Varðu 1Þ > 0 to be unrestricted, the APE would depend on<br />

d 1 =s 1 <strong>and</strong> a 1 =s 1 , <strong>and</strong> so we should just rescale u 1 to have unit variance. The variance<br />

<strong>and</strong> slope parameters are not separately identified, anyway.] The proper normalization<br />

for Varðu 1 Þ should be kept in mind, as two-step procedures, which we cover in<br />

the following paragraphs, only consistently estimate d 1 <strong>and</strong> a 1 up to scale; we have to<br />

do a little more work to obtain estimates <strong>of</strong> the APE. If y 2 is a mismeasured variable,<br />

we apparently cannot estimate the APE <strong>of</strong> interest: we would like to estimate the<br />

change in the response probability due to a change in y2 , but, without further assumptions,<br />

we can only estimate the e¤ect <strong>of</strong> changing y 2 .<br />

The most useful two-step approach is due to Rivers <strong>and</strong> Vuong (1988), as it leads<br />

to a simple test for endogeneity <strong>of</strong> y 2 . To derive the procedure, first note that, under<br />

joint normality <strong>of</strong> ðu 1 ; v 2 Þ, with Varðu 1 Þ¼1, we can write<br />

u 1 ¼ y 1 v 2 þ e 1<br />

ð15:42Þ<br />

where y 1 ¼ h 1 =t 2 2 , h 1 ¼ Covðv 2 ; u 1 Þ, t 2 2 ¼ Varðv 2Þ, <strong>and</strong> e 1 is independent <strong>of</strong> z <strong>and</strong><br />

v 2 (<strong>and</strong> therefore <strong>of</strong> y 2 ). Because <strong>of</strong> joint normality <strong>of</strong> ðu 1 ; v 2 Þ, e 1 is also normally

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