Enhanced Deep Blue aerosol retrieval algorithm: The second generation

dc.contributor.authorHsu, N. C.
dc.contributor.authorJeong, M.-J.
dc.contributor.authorBettenhausen, C.
dc.contributor.authorSayer, Andrew
dc.contributor.authorHansell, R.
dc.contributor.authorSeftor, C. S.
dc.contributor.authorHuang, J.
dc.contributor.authorTsay, S.-C.
dc.date.accessioned2024-04-29T17:01:14Z
dc.date.available2024-04-29T17:01:14Z
dc.date.issued2013-08-12
dc.description.abstractThe aerosol products retrieved using the Moderate Resolution Imaging Spectroradiometer (MODIS) collection 5.1 Deep Blue algorithm have provided useful information about aerosol properties over bright-reflecting land surfaces, such as desert, semiarid, and urban regions. However, many components of the C5.1 retrieval algorithm needed to be improved; for example, the use of a static surface database to estimate surface reflectances. This is particularly important over regions of mixed vegetated and nonvegetated surfaces, which may undergo strong seasonal changes in land cover. In order to address this issue, we develop a hybrid approach, which takes advantage of the combination of precalculated surface reflectance database and normalized difference vegetation index in determining the surface reflectance for aerosol retrievals. As a result, the spatial coverage of aerosol data generated by the enhanced Deep Blue algorithm has been extended from the arid and semiarid regions to the entire land areas. In this paper, the changes made in the enhanced Deep Blue algorithm regarding the surface reflectance estimation, aerosol model selection, and cloud screening schemes for producing the MODIS collection 6 aerosol products are discussed. A similar approach has also been applied to the algorithm that generates the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) Deep Blue products. Based upon our preliminary results of comparing the enhanced Deep Blue aerosol products with the Aerosol Robotic Network (AERONET) measurements, the expected error of the Deep Blue aerosol optical thickness (AOT) is estimated to be better than 0.05 + 20%. Using 10 AERONET sites with long-term time series, 79% of the best quality Deep Blue AOT values are found to fall within this expected error.
dc.description.sponsorshipThis work was supported by the NASA EOS program, managed by Hal Maring. The authors gratefully acknowledge the MODIS Characterization Support Team for their extensive efforts in maintaining the high radiometric quality of MODIS level 1 data. Appreciations also extend to Jeremy Warner and Rebecca Limbacher for their supports on the construction of the Deep Blue surface database. We would also like to express our gratitude to several AERONET PIs in establishing and maintaining the long-term stations used in this investigation.
dc.description.urihttps://onlinelibrary.wiley.com/doi/abs/10.1002/jgrd.50712
dc.format.extent20 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m2lwiw-mlks
dc.identifier.citationHsu, N. C., M.-J. Jeong, C. Bettenhausen, A. M. Sayer, R. Hansell, C. S. Seftor, J. Huang, and S.-C. Tsay. “Enhanced Deep Blue Aerosol Retrieval Algorithm: The Second Generation.” Journal of Geophysical Research: Atmospheres 118, no. 16 (2013): 9296–9315. https://doi.org/10.1002/jgrd.50712.
dc.identifier.urihttps://doi.org/10.1002/jgrd.50712
dc.identifier.urihttp://hdl.handle.net/11603/33411
dc.language.isoen_US
dc.publisherAGU
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC GESTAR II
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.subjectaerosol
dc.subjectretrieval
dc.subjectsatellite
dc.titleEnhanced Deep Blue aerosol retrieval algorithm: The second generation
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0001-9149-1789

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