4.7 Article

Spatial Surface Reflectance Retrievals for Visible/Shortwave Infrared Remote Sensing via Gaussian Process Priors

Journal

REMOTE SENSING
Volume 14, Issue 9, Pages -

Publisher

MDPI
DOI: 10.3390/rs14092183

Keywords

imaging spectroscopy; atmospheric correction; spatial correlation; optimal estimation

Funding

  1. Research and Technology Development Fund of the Jet Propulsion Laboratory, California Institute of Technology
  2. National Science Foundation (NSF) [DMS-1521676, DMS-1654083, DMS1953005]

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Remote Visible/Shortwave Infrared (VSWIR) imaging spectroscopy is a powerful tool for measuring the composition of Earth's surface. This study proposes an extension to the traditional estimation procedure by introducing atmospheric correlations into the multivariate Gaussian prior, which improves the predicted atmospheric fields and reduces bias in surface reflectance retrievals.
Remote Visible/Shortwave Infrared (VSWIR) imaging spectroscopy is a powerful tool for measuring the composition of Earth's surface over wide areas. This compositional information is captured by the spectral surface reflectance, where distinct shapes and absorption features indicate the chemical, bio- and geophysical properties of the materials in the scene. Estimating this surface reflectance requires removing the influence of atmospheric distortions caused by water vapor and particles. Traditionally reflectance is estimated by considering one location at a time, disentangling atmospheric and surface effects independently at all locations in a scene. However, this approach does not take advantage of spatial correlations between contiguous pixels. We propose an extension to a common Bayesian approach, Optimal Estimation, by introducing atmospheric correlations into the multivariate Gaussian prior. We show how this approach can be implemented as a small change to the traditional estimation procedure, thus limiting the additional computational burden. We demonstrate a simple version of the technique using simulations and multiple airborne radiance data sets. Our results show that the predicted atmospheric fields are smoother and more realistic than independent inversions given the assumption of spatial correlation and may reduce bias in the surface reflectance retrievals compared to post-process smoothing.

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