2011
DOI: 10.1016/j.csda.2011.03.003
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Improved interval estimation of long run response from a dynamic linear model: A highest density region approach

Abstract: This paper proposes a new method of interval estimation for the long run response (or elasticity) parameter from a general linear dynamic model. We employ the biascorrected bootstrap, in which small sample biases associated with the parameter estimators are adjusted in two stages of the bootstrap. As a means of bias-correction, we use alternative analytic and bootstrap methods. To take atypical properties of the long run elasticity estimator into account, the highest density region (HDR) method is adopted for … Show more

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Cited by 9 publications
(4 citation statements)
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References 34 publications
(61 reference statements)
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“…We estimated the conditional density of daily precipitation given total daily change of specific humidity (∆Q in Eq. 2) of TMEs entering the NE-US using the local polynomial density estimation with the R package 'hdrcde' (Kim et al, 2011). Figure 9 shows that as the daily moisture release (∆Q) by the TMEs increases, the daily precipitation increases with a shift in the conditional distribution that is marked beyond a threshold of ∆Q of about 3500 g kg-1.…”
Section: Tmes and Extreme Precipitationmentioning
confidence: 99%
“…We estimated the conditional density of daily precipitation given total daily change of specific humidity (∆Q in Eq. 2) of TMEs entering the NE-US using the local polynomial density estimation with the R package 'hdrcde' (Kim et al, 2011). Figure 9 shows that as the daily moisture release (∆Q) by the TMEs increases, the daily precipitation increases with a shift in the conditional distribution that is marked beyond a threshold of ∆Q of about 3500 g kg-1.…”
Section: Tmes and Extreme Precipitationmentioning
confidence: 99%
“…Highest density regions are of interest in Bayesian analysis in the formulation of "credibility regions" and "highest posterior density regions" (see e.g., Wei and Tanner 1990;Turkkan and Pham-Gia 1993;Chen and Shao 1999) and also for broader classical inference problems using "highest confidence density regions" (see e.g., Tian et al 2011). These regions are also used in forecasting problems to obtain a "prediction region" for an observable variable (see e.g., Hyndman 1995;Kim, Fraser and Hyndman 2011). In many statistical problems, interest will focus on a continuous observable value or unknown parameter, but there are certainly problems where a discrete random variable or parameter may be of interest, and in such cases the discrete version of the HDR is of interest.…”
Section: Introductionmentioning
confidence: 99%
“…(2)) of TME entering the N.E. USA using the local polynomial density estimation with the R package 'hdrcde' (Kim et al, 2011). Figure 9 shows that as the daily moisture release (∆Q) by the TME increases, the daily precipitation increases with a shift in the 15 conditional distribution that is marked beyond a threshold of ∆Q of about 3500 g/Kg.…”
Section: Tme and Extreme Precipitationmentioning
confidence: 99%