Spatial variability of the atmosphere over southern England, and its effect on scene-based atmospheric corrections
Spatial variability of the atmosphere over southern England, and its effect on scene-based atmospheric corrections
Earth observation data acquired in the optical region require atmospheric correction before they can be used quantitatively. Most operational methods of atmospheric correction assume that the atmospheric properties are uniform across the image, but this assumption is unlikely to be valid for large images. This study aims to characterize the spatial variation in atmospheric properties over a typical mid-latitude area (southern England), and to assess the errors that would result from applying a scene-based atmospheric correction to data collected under this variable atmosphere. Two key atmospheric properties – aerosol optical thickness (AOT) and precipitable water content (PWC) – are assessed over two clear days in June 2006, and results show an AOT range of approximately 0.1–0.5 and a PWC range of 1.5–3.0 cm. Radiative transfer modelling shows that errors in reflectance of up to 1.7 percentage points, and up to a 5% change in normalized difference vegetation index, can be caused by AOT variability, but that PWC variability has minimal effects. Sensitivity analyses also show that the high uncertainty of many data sources used to provide AOT values for atmospheric correction may also lead to significant errors in the resulting products. The spatial variability of the atmosphere cannot be ignored, and we are in need of operational, generic methods to perform a spatially variable atmospheric correction.
5198-5218
Wilson, R.T.
8c7289f8-8e43-4b2b-b1de-e3a733c48163
Milton, E.J.
f6cb5c0d-a5d4-47d7-860f-096de08e0c24
Nield, Joanna M.
173be2c5-b953-481a-abc4-c095e5e4b790
17 July 2014
Wilson, R.T.
8c7289f8-8e43-4b2b-b1de-e3a733c48163
Milton, E.J.
f6cb5c0d-a5d4-47d7-860f-096de08e0c24
Nield, Joanna M.
173be2c5-b953-481a-abc4-c095e5e4b790
Wilson, R.T., Milton, E.J. and Nield, Joanna M.
(2014)
Spatial variability of the atmosphere over southern England, and its effect on scene-based atmospheric corrections.
International Journal of Remote Sensing, 35 (13), .
(doi:10.1080/01431161.2014.939781).
Abstract
Earth observation data acquired in the optical region require atmospheric correction before they can be used quantitatively. Most operational methods of atmospheric correction assume that the atmospheric properties are uniform across the image, but this assumption is unlikely to be valid for large images. This study aims to characterize the spatial variation in atmospheric properties over a typical mid-latitude area (southern England), and to assess the errors that would result from applying a scene-based atmospheric correction to data collected under this variable atmosphere. Two key atmospheric properties – aerosol optical thickness (AOT) and precipitable water content (PWC) – are assessed over two clear days in June 2006, and results show an AOT range of approximately 0.1–0.5 and a PWC range of 1.5–3.0 cm. Radiative transfer modelling shows that errors in reflectance of up to 1.7 percentage points, and up to a 5% change in normalized difference vegetation index, can be caused by AOT variability, but that PWC variability has minimal effects. Sensitivity analyses also show that the high uncertainty of many data sources used to provide AOT values for atmospheric correction may also lead to significant errors in the resulting products. The spatial variability of the atmosphere cannot be ignored, and we are in need of operational, generic methods to perform a spatially variable atmospheric correction.
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e-pub ahead of print date: 17 July 2014
Published date: 17 July 2014
Organisations:
Geography & Environment
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Local EPrints ID: 365561
URI: http://eprints.soton.ac.uk/id/eprint/365561
ISSN: 0143-1161
PURE UUID: 03a5a405-63b3-48ab-a904-51e939e134ff
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Date deposited: 10 Jun 2014 12:12
Last modified: 15 Mar 2024 03:29
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Author:
R.T. Wilson
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