Multi-angle implementation of atmospheric correction for MODIS (MAIAC): 3. atmospheric correction
Multi-angle implementation of atmospheric correction for MODIS (MAIAC): 3. atmospheric correction
This paper describes the atmospheric correction (AC) component of the Multi-Angle Implementation of Atmospheric Correction algorithm (MAIAC) which introduces a new way to compute parameters of the Ross-Thick Li-Sparse (RTLS) Bi-directional reflectance distribution function (BRDF), spectral surface albedo and bidirectional reflectance factors (BRF) from satellite measurements obtained by the Moderate Resolution Imaging Spectroradiometer (MODIS). MAIAC uses a time series and spatial analysis for cloud detection, aerosol retrievals and atmospheric correction. It implements a moving window of up to 16 days of MODIS data gridded to 1 km resolution in a selected projection. The RTLS parameters are computed directly by fitting the cloud-free MODIS top of atmosphere (TOA) reflectance data stored in the processing queue. The RTLS retrieval is applied when the land surface is stable or changes slowly. In case of rapid or large magnitude change (as for instance caused by disturbance), MAIAC follows the MODIS operational BRDF/albedo algorithm and uses a scaling approach where the BRDF shape is assumed stable but its magnitude is adjusted based on the latest single measurement. To assess the stability of the surface, MAIAC features a change detection algorithm which analyzes relative change of reflectance in the Red and NIR bands during the accumulation period. To adjust for the reflectance variability with the sun-observer geometry and allow comparison among different days (view geometries), the BRFs are normalized to the fixed view geometry using the RTLS model. An empirical analysis of MODIS data suggests that the RTLS inversion remains robust when the relative change of geometry-normalized reflectance stays below 15%. This first of two papers introduces the algorithm, a second, companion paper illustrates its potential by analyzing MODIS data over a tropical rainforest and assessing errors and uncertainties of MAIAC compared to conventional MODIS products.
aerosols, maiac, modis, multi-angle implementation of atmospheric correcti, surface reflectance, time series, atmospheric correction
385-393
Lyapustin, Alexei I.
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Wang, Yujie
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Laszlo, Istvan
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Hilker, Thomas
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G.Hall, Forrest
411ff5b2-7da0-41c0-bf21-245a463e0fa7
Sellers, Piers J.
c9d7b8a6-3ed9-4e9f-9318-cc287e746315
Tucker, Compton J.
3aaff73d-aa1f-49c0-9d16-7099c218b274
Korkin, Sergey V.
4aff2ad9-46ff-412f-9ca4-043cfba83e72
December 2012
Lyapustin, Alexei I.
ee8fd005-4cb8-491c-a7c5-38d57a562608
Wang, Yujie
6915380d-4c23-4fef-a172-6880ddeff699
Laszlo, Istvan
d55edec7-ab6b-432c-9aa9-d7429966c96c
Hilker, Thomas
c7fb75b8-320d-49df-84ba-96c9ee523d40
G.Hall, Forrest
411ff5b2-7da0-41c0-bf21-245a463e0fa7
Sellers, Piers J.
c9d7b8a6-3ed9-4e9f-9318-cc287e746315
Tucker, Compton J.
3aaff73d-aa1f-49c0-9d16-7099c218b274
Korkin, Sergey V.
4aff2ad9-46ff-412f-9ca4-043cfba83e72
Lyapustin, Alexei I., Wang, Yujie, Laszlo, Istvan, Hilker, Thomas, G.Hall, Forrest, Sellers, Piers J., Tucker, Compton J. and Korkin, Sergey V.
(2012)
Multi-angle implementation of atmospheric correction for MODIS (MAIAC): 3. atmospheric correction.
Remote Sensing of Environment, 127, .
(doi:10.1016/j.rse.2012.09.002).
Abstract
This paper describes the atmospheric correction (AC) component of the Multi-Angle Implementation of Atmospheric Correction algorithm (MAIAC) which introduces a new way to compute parameters of the Ross-Thick Li-Sparse (RTLS) Bi-directional reflectance distribution function (BRDF), spectral surface albedo and bidirectional reflectance factors (BRF) from satellite measurements obtained by the Moderate Resolution Imaging Spectroradiometer (MODIS). MAIAC uses a time series and spatial analysis for cloud detection, aerosol retrievals and atmospheric correction. It implements a moving window of up to 16 days of MODIS data gridded to 1 km resolution in a selected projection. The RTLS parameters are computed directly by fitting the cloud-free MODIS top of atmosphere (TOA) reflectance data stored in the processing queue. The RTLS retrieval is applied when the land surface is stable or changes slowly. In case of rapid or large magnitude change (as for instance caused by disturbance), MAIAC follows the MODIS operational BRDF/albedo algorithm and uses a scaling approach where the BRDF shape is assumed stable but its magnitude is adjusted based on the latest single measurement. To assess the stability of the surface, MAIAC features a change detection algorithm which analyzes relative change of reflectance in the Red and NIR bands during the accumulation period. To adjust for the reflectance variability with the sun-observer geometry and allow comparison among different days (view geometries), the BRFs are normalized to the fixed view geometry using the RTLS model. An empirical analysis of MODIS data suggests that the RTLS inversion remains robust when the relative change of geometry-normalized reflectance stays below 15%. This first of two papers introduces the algorithm, a second, companion paper illustrates its potential by analyzing MODIS data over a tropical rainforest and assessing errors and uncertainties of MAIAC compared to conventional MODIS products.
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More information
Accepted/In Press date: 1 September 2012
e-pub ahead of print date: 29 September 2012
Published date: December 2012
Keywords:
aerosols, maiac, modis, multi-angle implementation of atmospheric correcti, surface reflectance, time series, atmospheric correction
Organisations:
Earth Surface Dynamics
Identifiers
Local EPrints ID: 384694
URI: http://eprints.soton.ac.uk/id/eprint/384694
ISSN: 0034-4257
PURE UUID: fc0a7f52-f636-4fca-8567-092b21f3f1a1
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Date deposited: 15 Apr 2016 15:40
Last modified: 14 Mar 2024 22:02
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Contributors
Author:
Alexei I. Lyapustin
Author:
Yujie Wang
Author:
Istvan Laszlo
Author:
Thomas Hilker
Author:
Forrest G.Hall
Author:
Piers J. Sellers
Author:
Compton J. Tucker
Author:
Sergey V. Korkin
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