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This section introduces measurement models for quantitative as well as qualitative fore-casts. In these state-space models, the responses of a day are seen as draws from the population distribution of expectations, which changes from day to day. The goal is to estimate its shape on a given day.

The state-space modeling approach is a natural choice for this problem: First, within its framework, I can easily formalize that the responses on a specific day are noisy signals about the population distribution of forecasts. Second, it allows us to account for variation in the signal precision arising from a changing number of responses per day. Third, the approach naturally overcomes the hurdle of the missing values I observe when no survey responses are collected. Fourth, I can easily augment the model with additional measurement variables such as financial asset prices and relate them to the dynamics in the population distribution of forecasts.

1.2.1 Quantitative Forecasts

Denoting the point expectation of respondent i stated on day t by yit, and the average across the responses collected on day t by y¯t = 1/ntP

iyit, I set up the following state-space model

¯

yt = µtt, εtiid∼ N(0, σε2/nt), (1.1) µt+1 = µtt+1, ηt+1 iid∼ N(0, ση2). (1.2) Given that σ2ε and ση2 are constant, interest lies in estimating how µt, the mean of the population distribution of forecasts, changes over time. Estimation is based on Maximum Likelihood and the Kalman Filter. Its details are outlined in Appendix 1.A.

I next discuss the model: The measurement equation (eq. 1.1) implicitly assumes that the individual responses on daytare draws from a distribution with meanµtand variance σε2, such that the average response has variance σε2/nt, reflecting that the quality of the signal y¯t for µt increases with the number of responses.

The implicit assumption about the individual responses is not particularly restrictive as it is compatible with individual responses that have the following structure

yitt+uiit,

where µt is a common trend, ui is an individual random effect with ui

iid∼ (E[ui] = 0, V[ui] = σu2), and ξit is an individual disturbance with ξit iid∼ (E[ξit] = 0, V[ξit] = σ2ξ

it).

The random effect (ui) reflects that some respondents are generally more or less optimistic about the future, thus permanently over- or under-predicting economic variables. The individual disturbances (ξit) captures that, despite the overlap between the information respondents have and the interpretations they derive from it, differences typically exist.1 From these assumptions it immediately follows that the average response y¯t has mean µt and variance σε2/nt = (σu22ξ)/nt, as I state in equation (1.1). Moreover, approximate normality of the measurement equation (eq. 1.1) arises if either (a) ntis reasonably large according to the Lindeberg-Levy central limit theorem, or if (b) the distributions of the two disturbancesuiandξitare normal themselves. Contrary to my assumption of a serially uncorrelated measurement error εt, a random effectui may induce correlation among any pair of measurement errorsy¯t−µt = 1/ntP

(uiit)andy¯t+h−µt+h = 1/ntP

(uiit+h), provided that there is significant overlap in the samples collected at t and at t+h, such that the same random effects are featured in both samples. As respondents reply (at most) once in a survey period, there can be no overlap for small values of h. If the value of h implies that I compare different survey waves, provided that respondents systematically respond on specific days of the survey period, the random effect may seriously invalidate the assumption of no serial correlation in the measurement errors. As this does not hold in the data I have at hand, I conjecture that the assumption is a reasonable simplification.

The state equation (eq. 1.2) has the structure of a random walk. It reflects that with no other information at hand, my best estimate of tomorrow’s state of expectations is today’s. Using the Kalman Filter, I will revise this estimate after observing tomorrow’s responses.2 Later in this article, I will use regularly observed data such as the change in the price of certain financial assets to improve my estimate of the state of expectations.

1see the relatively recent strand of literature about forecast disagreement, e.g. Lahiri and Sheng (2008) or Mankiw, Reis, and Wolfers (2004).

2The random walk assumption does not imply that expectations are not influenced by other observable data and that I cannot learn from these data about the state of expectations.

My baseline model can be extended in several directions: One interesting avenue is to relax the assumption that the measurement error (εt) is homoscedastic and thus capture that the disagreement of expectations may change over time. Another is to relax the homoscedasticity of the state disturbance (ηt), e.g. by allowing that shocks may either come from a business-as-usual distribution with moderate variance or from an major-event distribution with a large variance.

1.2.1.1 Adding another measurement variable

Recognizing that surveys do not collect survey responses all the time, we may want to use additional data that are observed on a regular basis to estimate changes in the latent distribution of survey forecasts. The additional data I have in mind are variables that indirectly measure (market) expectations. For example, long-term bond yields impound expectations about future short-term nominal and real interest rates and about inflation.

To benefit from such indirect measures of expectations (denoted by xt), I augment the measurement equation (eq. 1.1) in the following way:

"

and assume that the measurement error εx,t has variance σ2x and that it is serially uncor-related and uncoruncor-related at all leads and lags with both the measurement errorεtand the state disturbance ηt.

In equation (1.3), I assume that xt is related to the day-over-day change in µt, which implies that xt must be stationary. Non-stationary financial asset prices will thus have to be transformed to stationarity, either by taking the day-over-day price change or the day-over-day return. If I were to assume that xt loads on the level of µt, the unit root in µt (see eq. 1.2) would require that xt and y¯t are cointegrated - an overly restrictive assumption.

The way I link the additional measurement to the state variable is identical to Ghysels and Wright (2009). The idea is that the same economic news that impact on economic expectations are likely to be “impounded in financial asset prices” (Ghysels and Wright, 2009, p.504), such that the additional variable provides a noisy signal about the change in the state variable.

1.2.2 Qualitative Forecasts

Suppose instead of point forecasts, as in the case of the empirical application, I observe qualitative forecasts. Individual responses are either “will rise”, “will stay the same”, or

“will fall” and can thus be seen as draws from a multinomial distribution. Denoting by y¯t a two-element column vector holding the shares of “will rise” and “will fall” responses on day t3, I set up the following non-linear state space model:

¯

whereηti.i.d.∼ N(0,Ση),andεt is a serially independent disturbance vector with mean zero and variance

Interest lies in estimating the path of πt, the vector of the population probabilities for a “will rise” and a “will fall” response. This is a dual estimation problem as it involves the estimation of both the model parameters and the path of the state variables. Pro-vided with candidate model parameters, the Unscented Kalman Filter (e.g. Wan and Van Der Merwe, 2000) estimates the path of the state variables, which is in turn used to compute the model likelihood. Parameter estimates are obtained by maximizing the like-lihood with respect to the model parameters (maximum likelike-lihood estimation). Details are given in Appendix 1.B.

To understand the model, note that the mean and variance of the measurement equation (1.4) follow from the assumption that the responses are independent and identically dis-tributed draws from a multinomial distribution with πR,t being the probability of a “will rise” and πF,t being the probability of a a “will fall” response.

Finally, it is interesting to note that the state-space model specified by equations (1.4-1.7) implies that the vector of log-odds ratios with elementsln(πR,tS,t)andln(πF,tS,t), evolves according to the bivariate random walk specified in equation (1.6).

3Note, that in equation (1.4), I have not included the share of “stay the same” responses, since it is linearly determined from the two other shares as 11/ntP

i

1(yit=’rise’)+1(yit=’fall’)

. A similar argument holds for the probability of a “stay the same” response.

1.2.2.1 Adding another measurement variable

As for the model for point forecasts of section 1.2.1, we may want to use additional daily variables to estimate changes in the latent distribution of survey forecasts. I augment the measurement equation (1.4) in the following way:

"

and assume that the second measurement’s error εx,t has variance σx2, and that it is serially independent and independent at all leads and lags from the measurement error vector εt and the state disturbance vector ηt. Similar to the model for point forecasts with an additional measurement variable, xt is related to the day-over-day change in the difference of the two state variables. Thus, xt must be stationary.