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Article: Improvement of dark object method in atmospheric correction of hyperspectral remotely sensed data
Title | Improvement of dark object method in atmospheric correction of hyperspectral remotely sensed data |
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Authors | |
Keywords | Atmospheric correction Dark object Hyper spectral Hyperion Remote sensing |
Issue Date | 2008 |
Citation | Science in China, Series D: Earth Sciences, 2008, v. 51, n. 3, p. 349-356 How to Cite? |
Abstract | The existing methods in atmospheric correction of hyperspectral data usually focus on removing the effects of water vapor and other absorptive gases, while this paper mainly studies the method of removing the influence of the aerosol and the water vapor simultaneously. Because the hyperspectral data has a larger number of bands, the conventional dark object method cannot be applied to the atmospheric correction of the hyperspectral data which can be improved, as described in this paper, by adequately making use of spectral characteristics of the hyperspectral data with an iterative correction during the whole process. The effects of the aerosol and water vapor are eliminated at the same time finally. The improved dark object method is used to do the atomospheric correction of the Hyperion data in Yanzhou, Shandong Province as an example. And the result indicates that it can correct the atmospheric influence of the hyperspectral data quickly and remarkably. © Science in China Press 2008. |
Persistent Identifier | http://hdl.handle.net/10722/321343 |
ISSN | 2011 Impact Factor: 1.588 |
ISI Accession Number ID |
DC Field | Value | Language |
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dc.contributor.author | Zhao, Xiang | - |
dc.contributor.author | Liang, Shun Lin | - |
dc.contributor.author | Liu, Su Hong | - |
dc.contributor.author | Wang, Jin Di | - |
dc.contributor.author | Qin, Jun | - |
dc.contributor.author | Li, Qing | - |
dc.contributor.author | Li, Xiao Wen | - |
dc.date.accessioned | 2022-11-03T02:18:16Z | - |
dc.date.available | 2022-11-03T02:18:16Z | - |
dc.date.issued | 2008 | - |
dc.identifier.citation | Science in China, Series D: Earth Sciences, 2008, v. 51, n. 3, p. 349-356 | - |
dc.identifier.issn | 1006-9313 | - |
dc.identifier.uri | http://hdl.handle.net/10722/321343 | - |
dc.description.abstract | The existing methods in atmospheric correction of hyperspectral data usually focus on removing the effects of water vapor and other absorptive gases, while this paper mainly studies the method of removing the influence of the aerosol and the water vapor simultaneously. Because the hyperspectral data has a larger number of bands, the conventional dark object method cannot be applied to the atmospheric correction of the hyperspectral data which can be improved, as described in this paper, by adequately making use of spectral characteristics of the hyperspectral data with an iterative correction during the whole process. The effects of the aerosol and water vapor are eliminated at the same time finally. The improved dark object method is used to do the atomospheric correction of the Hyperion data in Yanzhou, Shandong Province as an example. And the result indicates that it can correct the atmospheric influence of the hyperspectral data quickly and remarkably. © Science in China Press 2008. | - |
dc.language | eng | - |
dc.relation.ispartof | Science in China, Series D: Earth Sciences | - |
dc.subject | Atmospheric correction | - |
dc.subject | Dark object | - |
dc.subject | Hyper spectral | - |
dc.subject | Hyperion | - |
dc.subject | Remote sensing | - |
dc.title | Improvement of dark object method in atmospheric correction of hyperspectral remotely sensed data | - |
dc.type | Article | - |
dc.description.nature | link_to_subscribed_fulltext | - |
dc.identifier.doi | 10.1007/s11430-007-0149-y | - |
dc.identifier.scopus | eid_2-s2.0-40349099991 | - |
dc.identifier.volume | 51 | - |
dc.identifier.issue | 3 | - |
dc.identifier.spage | 349 | - |
dc.identifier.epage | 356 | - |
dc.identifier.eissn | 1862-2801 | - |
dc.identifier.isi | WOS:000253527000004 | - |