Estimation of AOD Under Uncertainty: An Approach for Hyperspectral Airborne Data
A key parameter for atmospheric correction (AC) is Aerosol Optical Depth (AOD), which is often estimated from sensor radiance (Lrs,t(λ)). Noise, the dependency on surface type, viewing and illumination geometry cause uncertainty in AOD inference. We propose a method that determines pre-estimates of...
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doaj-cfc97524d773474fb90b24a4cd91e4d82020-11-25T00:29:42ZengMDPI AGRemote Sensing2072-42922018-06-0110694710.3390/rs10060947rs10060947Estimation of AOD Under Uncertainty: An Approach for Hyperspectral Airborne DataNitin Bhatia0Valentyn A. Tolpekin1Alfred Stein2Ils Reusen3Remote Sensing Unit, Flemish Institute for Technological Research, 2400 Mol, BelgiumDepartment of Earth Observation Science, Faculty of Geo-Information Science and Earth Observation, University of Twente, 7500 AE Enschede, The NetherlandsDepartment of Earth Observation Science, Faculty of Geo-Information Science and Earth Observation, University of Twente, 7500 AE Enschede, The NetherlandsRemote Sensing Unit, Flemish Institute for Technological Research, 2400 Mol, BelgiumA key parameter for atmospheric correction (AC) is Aerosol Optical Depth (AOD), which is often estimated from sensor radiance (Lrs,t(λ)). Noise, the dependency on surface type, viewing and illumination geometry cause uncertainty in AOD inference. We propose a method that determines pre-estimates of surface reflectance (ρt,pre) where effects associated with Lrs,t(λ) are less influential. The method identifies pixels comprising pure materials from ρt,pre. AOD values at the pure pixels are iteratively estimated using l2-norm optimization. Using the adjacency range function, the AOD is estimated at each pixel. We applied the method on Hyperspectral Mapper and Airborne Prism Experiment instruments for experiments on synthetic data and on real data. To simulate real imaging conditions, noise was added to the data. The estimation error of the AOD is minimized to 0.06–0.08 with a signal-to-reconstruction-error equal to 35 dB. We compared the proposed method with a dense dark vegetation (DDV)-based state-of-the-art method. This reference method, resulted in a larger variability in AOD estimates resulting in low signal-to-reconstruction-error between 5–10 dB. For per-pixel estimation of AOD, the performance of the reference method further degraded. We conclude that the proposed method is more precise than the DDV methods and can be extended to other AC parameters.http://www.mdpi.com/2072-4292/10/6/947aerosol optical depthuncertaintysensitivityadjacency rangeatmospheric correctionhyperspectral unmixing |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Nitin Bhatia Valentyn A. Tolpekin Alfred Stein Ils Reusen |
spellingShingle |
Nitin Bhatia Valentyn A. Tolpekin Alfred Stein Ils Reusen Estimation of AOD Under Uncertainty: An Approach for Hyperspectral Airborne Data Remote Sensing aerosol optical depth uncertainty sensitivity adjacency range atmospheric correction hyperspectral unmixing |
author_facet |
Nitin Bhatia Valentyn A. Tolpekin Alfred Stein Ils Reusen |
author_sort |
Nitin Bhatia |
title |
Estimation of AOD Under Uncertainty: An Approach for Hyperspectral Airborne Data |
title_short |
Estimation of AOD Under Uncertainty: An Approach for Hyperspectral Airborne Data |
title_full |
Estimation of AOD Under Uncertainty: An Approach for Hyperspectral Airborne Data |
title_fullStr |
Estimation of AOD Under Uncertainty: An Approach for Hyperspectral Airborne Data |
title_full_unstemmed |
Estimation of AOD Under Uncertainty: An Approach for Hyperspectral Airborne Data |
title_sort |
estimation of aod under uncertainty: an approach for hyperspectral airborne data |
publisher |
MDPI AG |
series |
Remote Sensing |
issn |
2072-4292 |
publishDate |
2018-06-01 |
description |
A key parameter for atmospheric correction (AC) is Aerosol Optical Depth (AOD), which is often estimated from sensor radiance (Lrs,t(λ)). Noise, the dependency on surface type, viewing and illumination geometry cause uncertainty in AOD inference. We propose a method that determines pre-estimates of surface reflectance (ρt,pre) where effects associated with Lrs,t(λ) are less influential. The method identifies pixels comprising pure materials from ρt,pre. AOD values at the pure pixels are iteratively estimated using l2-norm optimization. Using the adjacency range function, the AOD is estimated at each pixel. We applied the method on Hyperspectral Mapper and Airborne Prism Experiment instruments for experiments on synthetic data and on real data. To simulate real imaging conditions, noise was added to the data. The estimation error of the AOD is minimized to 0.06–0.08 with a signal-to-reconstruction-error equal to 35 dB. We compared the proposed method with a dense dark vegetation (DDV)-based state-of-the-art method. This reference method, resulted in a larger variability in AOD estimates resulting in low signal-to-reconstruction-error between 5–10 dB. For per-pixel estimation of AOD, the performance of the reference method further degraded. We conclude that the proposed method is more precise than the DDV methods and can be extended to other AC parameters. |
topic |
aerosol optical depth uncertainty sensitivity adjacency range atmospheric correction hyperspectral unmixing |
url |
http://www.mdpi.com/2072-4292/10/6/947 |
work_keys_str_mv |
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