Reconciling satellite-derived atmospheric properties with fine-resolution land imagery: Insights for atmospheric correction
dc.contributor.author | Zelazowski, Przemyslaw | |
dc.contributor.author | Sayer, Andrew | |
dc.contributor.author | Thomas, Gareth E. | |
dc.contributor.author | Grainger, Roy G. | |
dc.date.accessioned | 2024-04-29T17:01:28Z | |
dc.date.available | 2024-04-29T17:01:28Z | |
dc.date.issued | 2011-09-30 | |
dc.description.abstract | This paper investigates to what extent satellite measurements of atmospheric properties can be reconciled with fine-resolution land imagery, in order to improve the estimates of surface reflectance through physically based atmospheric correction. The analysis deals with mountainous area (Landsat scene of Peruvian Amazon/Andes, 72°E and 13°S), where the atmosphere is highly variable. Data from satellite sensors were used for characterization of the key atmospheric constituents: total water vapor (TWV), aerosol optical depth (AOD), and total ozone. Constituent time series revealed the season-dependent mean state of the atmosphere and its variability. Discrepancies between AOD from the Advanced Along-Track Scanning Radiometer (AATSR) and Moderate Resolution Imaging Spectroradiometer (MODIS) highlighted substantial uncertainty of atmospheric aerosol properties. The distribution of TWV and AOD over a Landsat scene was found to be exponentially related to ground elevation (mean R² of 0.82 and 0.29, respectively). In consequence, the atmosphere-induced and seasonally varying bias of the top-of-atmosphere signal was also elevation dependent (e.g., mean Normalized Difference Vegetation Index bias at 500 m was 0.06 and at 4000 m was 0.01). We demonstrate that satellite measurements of key atmospheric constituents can be downscaled and gap filled with the proposed “background + anomalies” approach, to allow for a better compatibility with fine-resolution land surface imagery. Older images (i.e., predating the MODIS/ATSR era), without coincident atmospheric data, can be corrected using climatologies derived from time series of satellite retrievals. Averaging such climatologies over space compromises the quality of correction result to a much greater degree than averaging them over time. We conclude that the quality of both recent and older fine-resolution land surface imagery can be improved with satellite-based atmospheric data acquired to date. | |
dc.description.sponsorship | We are very grateful to Giles Foody, Yadvinder Malhi, Soo Chin Liew, and two anonymous reviewers for useful suggestions on the manuscript. The research was supported financially by the Blue Moon Foundation. | |
dc.description.uri | https://onlinelibrary.wiley.com/doi/abs/10.1029/2010JD015488 | |
dc.format.extent | 15 pages | |
dc.genre | journal articles | |
dc.identifier | doi:10.13016/m2zb50-dpn3 | |
dc.identifier.citation | Zelazowski, Przemyslaw, Andrew M. Sayer, Gareth E. Thomas, and Roy G. Grainger. “Reconciling Satellite-Derived Atmospheric Properties with Fine-Resolution Land Imagery: Insights for Atmospheric Correction.” Journal of Geophysical Research: Atmospheres 116, no. D18 (2011). https://doi.org/10.1029/2010JD015488. | |
dc.identifier.uri | https://doi.org/10.1029/2010JD015488 | |
dc.identifier.uri | http://hdl.handle.net/11603/33433 | |
dc.language.iso | en_US | |
dc.publisher | AGU | |
dc.relation.isAvailableAt | The University of Maryland, Baltimore County (UMBC) | |
dc.relation.ispartof | UMBC GESTAR II | |
dc.rights | ©2018. American Geophysical Union. All Rights Reserved | |
dc.subject | aerosol | |
dc.subject | AOD | |
dc.subject | atmospheric correction | |
dc.subject | ozone | |
dc.subject | satellite measurements | |
dc.subject | water vapor | |
dc.title | Reconciling satellite-derived atmospheric properties with fine-resolution land imagery: Insights for atmospheric correction | |
dc.type | Text | |
dcterms.creator | https://orcid.org/0000-0001-9149-1789 |
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