2018
DOI: 10.1016/j.jqsrt.2018.01.008
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Bayesian estimation of seasonal course of canopy leaf area index from hyperspectral satellite data

Abstract: In this paper, Bayesian inversion of a physically-based forest reflectance model is investigated to estimate of boreal forest canopy leaf area index (LAI) from EO-1 Hyperion hyperspectral data. The data consist of multiple forest stands with different species compositions and structures, imaged in three phases of the growing season. The Bayesian estimates of canopy LAI are compared to reference estimates based on on a spectral vegetation index. The forest reflectance model contains also other unknown variables… Show more

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Cited by 21 publications
(5 citation statements)
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“…In LLEVAP the evaporation of an organic compound i is controlled by the difference in its gas-phase concentration C i and the equilibrium concentration C eq,i (Vesala et al, 1997;Lehtinen and Kulmala, 2003), equivalent to the gas-phase diffusional gradient between the infinite distance and particle surface, respectively. Therefore, the mass transport between the gas and the particle phases is assumed to be the limiting phenomenon and the diffusion timescales within the particle are assumed to be negligible.…”
Section: Process Modelsmentioning
confidence: 99%
“…In LLEVAP the evaporation of an organic compound i is controlled by the difference in its gas-phase concentration C i and the equilibrium concentration C eq,i (Vesala et al, 1997;Lehtinen and Kulmala, 2003), equivalent to the gas-phase diffusional gradient between the infinite distance and particle surface, respectively. Therefore, the mass transport between the gas and the particle phases is assumed to be the limiting phenomenon and the diffusion timescales within the particle are assumed to be negligible.…”
Section: Process Modelsmentioning
confidence: 99%
“…where f b is the fraction of direct (non-diffuse) radiation; τ is the canopy transmittance (transmitted PAR/incident PAR); K is the extinction coefficient; χ is the leaf angle distribution, which is defined as the ratio of the horizontal to vertical axes of the ellipsoidal leaf distribution [30]; and θ is the solar zenith angle. Because the obtained parameters are inclusive of the non-photosynthetic component and aggregation effects, the obtained LAI is calculated as the LAI e [33][34][35].…”
Section: Plot-level Data Estimatesmentioning
confidence: 99%
“…While physical uncertainty is likely more of interest to the user community, exploration of theoretical uncertainty can help understand sources of physical uncertainty and improve LAI estimation. Bayesian approaches could provide theoretical uncertainty measures from posterior distribution and concurrent estimation of LAI based on uncertainty of input parameters [96,177,216,217]. Han and Qu [177] and Qu et al [217] used Bayesian approaches to conclude that the addition of high-resolution remote sensing observation data improved LAI estimation models and increase model reliability.…”
Section: The Uncertainty Of Lai Estimationmentioning
confidence: 99%