Reconciling satellite-derived atmospheric properties with fine-resolution land imagery: Insights for atmospheric correction

dc.contributor.authorZelazowski, Przemyslaw
dc.contributor.authorSayer, Andrew
dc.contributor.authorThomas, Gareth E.
dc.contributor.authorGrainger, Roy G.
dc.date.accessioned2024-04-29T17:01:28Z
dc.date.available2024-04-29T17:01:28Z
dc.date.issued2011-09-30
dc.description.abstractThis 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.sponsorshipWe 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.urihttps://onlinelibrary.wiley.com/doi/abs/10.1029/2010JD015488
dc.format.extent15 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m2zb50-dpn3
dc.identifier.citationZelazowski, 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.urihttps://doi.org/10.1029/2010JD015488
dc.identifier.urihttp://hdl.handle.net/11603/33433
dc.language.isoen_US
dc.publisherAGU
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC GESTAR II
dc.rights©2018. American Geophysical Union. All Rights Reserved
dc.subjectaerosol
dc.subjectAOD
dc.subjectatmospheric correction
dc.subjectozone
dc.subjectsatellite measurements
dc.subjectwater vapor
dc.titleReconciling satellite-derived atmospheric properties with fine-resolution land imagery: Insights for atmospheric correction
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0001-9149-1789

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