2006
DOI: 10.1109/lgrs.2005.856755
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A Bayesian Estimator for Linear Calibration Error Effects in Thermal Remote Sensing

Abstract: Abstract-The Bayesian Land Surface Temperature estimator previously developed has been extended to include the effects of imperfectly known gain and offset calibration errors. It is possible to treat both gain and offset as nuisance parameters and, by integrating over an uninformitave range for their magnitudes, eliminate the dependence of surface temperature and emissivity estimates upon the exact calibration error.

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Cited by 5 publications
(2 citation statements)
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“…Even though the posterior probability for surface T is a closed-form expression, this procedure is computationally intensive. Moreover, extensions to the estimator -such as, for example, a more careful treatment of the forward model, or incorporation of calibration error effects (Morgan 2006) -may deprive us of the comfort of the closed-form solution. The MAP criterion for an estimator promises to dramatically reduce the number of CPU cycles expended per LST estimate, and may yet preserve the ability to rely upon closed-form solutions.…”
Section: Lst Algorithmsmentioning
confidence: 99%
See 1 more Smart Citation
“…Even though the posterior probability for surface T is a closed-form expression, this procedure is computationally intensive. Moreover, extensions to the estimator -such as, for example, a more careful treatment of the forward model, or incorporation of calibration error effects (Morgan 2006) -may deprive us of the comfort of the closed-form solution. The MAP criterion for an estimator promises to dramatically reduce the number of CPU cycles expended per LST estimate, and may yet preserve the ability to rely upon closed-form solutions.…”
Section: Lst Algorithmsmentioning
confidence: 99%
“…We begin by adapting the analysis of Morgan (2005Morgan ( , 2006 to obtain the prior probability for surface meteorological range VSBY and use it to construct posterior probabilities marginalized over a range of VSBY. The starting point is the apparently trivial observation that the meteorological range is a length.…”
Section: Appendix B Insensitivity Of Lst Estimates To Meteorologicalmentioning
confidence: 99%