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Titlebook: Remote Sensing of the Earth from Space: Atmospheric Correction; Kirill Y. Kondratyev,Vladimir V. Kozoderov,Oleg I. Book 1992 A. P. Kostrov

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書(shū)目名稱(chēng)Remote Sensing of the Earth from Space: Atmospheric Correction
編輯Kirill Y. Kondratyev,Vladimir V. Kozoderov,Oleg I.
視頻videohttp://file.papertrans.cn/827/826946/826946.mp4
圖書(shū)封面Titlebook: Remote Sensing of the Earth from Space: Atmospheric Correction;  Kirill Y. Kondratyev,Vladimir V. Kozoderov,Oleg I. Book 1992 A. P. Kostrov
描述The monograph being proposed for the English-speaking research community is concentrated on the atmospheric correction of satellite images as a part of thematic interpretation procedures while processing remote sensing data. For linguistic reasons a large section of the community may have been unaware of the progress made in Russia in this field of science and technology. Meanwhile, Russia was the first country to launch the first artificial satellite in 1957 and to obtain from space for the first time spectra of the Earth‘s atmosphere in the 1960‘s. New applications of the radiation transfer theory for the atmosphere- underlying surface system appeared first in Russia in the 1970‘s. Direct and in- verse problems of the atmospheric optics were then formulated giving the scientific basis for studies of natural resources from space. Since that time new mathematical treatments for the atmospheric correction procedures have been widely developed in Russia, including both analytical and numerical tech- niques to simulate spectral, angular, and spatial distributions of the outgoing radiation in visual and infrared regions. The authors of the book were at the beginning of the scientific a
出版日期Book 1992
關(guān)鍵詞Aerosol; Atmosph?rische Korrektur; Interpretation von Satellitenphotos; Space-born information; atmosphe
版次1
doihttps://doi.org/10.1007/978-3-642-76747-0
isbn_softcover978-3-642-76749-4
isbn_ebook978-3-642-76747-0
copyrightA. P. Kostrova, Moscow 1992
The information of publication is updating

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The Effect of Horizontal Inhomogeneities of the Underlying Surface on the Scalar Transfer Function wed at different angles and with different combinations of objects in a given scene, will be different. This is determined by the horizontal inhomogeneity of the atmosphere and Earth’s surface as well as by the different extent of non-orthotropicity of natural objects.
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