Abstract

Airborne and orbital imaging spectroscopy can facilitate the quantification of chemical and physical attributes of surface materials through analysis of spectral signatures. Prior to analysis, estimates of surface reflectance must be inferred from radiance measurements in a process known as atmospheric correction, which compensates for the distortion of the electromagnetic signal by the atmosphere. Inaccuracies in the correction process can alter characteristic spectral signatures, leading to subsequent mischaracterization of surface properties. Global observations pose new challenges for mapping surface composition, as varied atmospheric conditions and surface biomes challenge traditional atmospheric correction methods. Recent work adopted an optimal estimation (OE) approach for retrieving surface reflectance from observed radiance measurements, providing the reflectance estimates with a posterior probability. This work incorporates these input probabilities to improve the accuracy of surface feature measurements. We demonstrate this using a generic feature-fitting method that is applicable to a wide range of Earth surface studies including geology, ecosystem studies, hydrology and urban studies. Specifically, we use a probabilistic framework based on generalized Tikhonov-regularized least squares, a rigorous formulation for appropriate weighting of features by their observation uncertainty and leveraging of prior knowledge of material abundance for improving estimation accuracy. We demonstrate the validity of this procedure and quantify the increase in model performance by simulating expected accuracies in the reflectance estimation. To evaluate global uncertainties in mineral estimation, we simulate observations representative of the expected global range of atmospheric water vapor and aerosol levels, and characterize the sensitivity of our procedure to those quantities.

Highlights

  • Mapping Earth's surface with imaging spectrometers has a long history of notable scientific discoveries, as the systematic advantages of remote-sensing technologies allow frequent spatially-continuous, and high-resolution information about the surface to be collected over large scales

  • In this experiment we demonstrated optimal estimation (OE)'s performance for simulta­ neously retrieving surface reflectance and atmospheric parameters from radiance observations that are simulated to represent global variability in atmospheric conditions

  • We show how uncertainty predictions from the surface reflectance retrieval can be leveraged to achieve an increase in prediction performance for surface composition maps, and propa­ gated to report the derived geophysical quantities with predicted un­ certainties

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Summary

Introduction

Mapping Earth's surface with imaging spectrometers has a long history of notable scientific discoveries, as the systematic advantages of remote-sensing technologies allow frequent spatially-continuous, and high-resolution information about the surface to be collected over large scales. Recent achievements in the fields of ecology, agriculture, and environmental monitoring used imaging spectroscopy to resolve scientific questions on broad spatial and temporal scales (Ustin et al, 2004) While historically most such investigations have relied on regional airborne campaigns, in the near future orbital earth observing imaging spectrometers will provide frequent data with global coverage. As the quantity of interest (QOI) for mapping surface properties is the surface reflectance, an atmospheric correction routine is needed to compensate for the atmosphere's dis­ tortion of the observed signal (Gao et al, 1993) This is usually done based on radiative transfer equations which provide a mathematical model for the physics of electromagnetic radiation passing through the atmosphere. Other atmospheric correction methodologies might rely only on empirical data collected from the scene, or combine in-situ data with radiative transfer (Carmon and Ben-Dor, 2018a; Pelta et al, 2019)

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