Hyperspectral imaging data have been collected with different types of imaging spectrometers from aircraft and satellite platforms since the mid-1980s. Because the solar radiation on the sun-surface-sensor path in the 0.4-2.5 Β΅m visible and near-IR spectral regions is subject to absorption and scatt
β¦ LIBER β¦
Decoupling error for the atmospheric correction in ocean color remote sensing algorithms
β Scribed by Peng-Wang Zhai; Yongxiang Hu; Charles R. Trepte; Patricia L. Lucker; Damien B. Josset
- Publisher
- Elsevier Science
- Year
- 2010
- Tongue
- English
- Weight
- 600 KB
- Volume
- 111
- Category
- Article
- ISSN
- 0022-4073
No coin nor oath required. For personal study only.
π SIMILAR VOLUMES
Atmospheric correction algorithms for hy
β
Bo-Cai Gao; Marcos J. Montes; Curtiss O. Davis; Alexander F.H. Goetz
π
Article
π
2009
π
Elsevier Science
π
English
β 544 KB
Evaluation of shortwave infrared atmosph
β
P. Jeremy Werdell; Bryan A. Franz; Sean W. Bailey
π
Article
π
2010
π
Elsevier Science
π
English
β 1019 KB
Estimated corrections for the atmosphere
β
D.A. Usikov; M.N. Fomenkova
π
Article
π
1987
π
Elsevier Science
π
English
β 299 KB
The use of an improved atmospheric corre
β
D. G. Hadjimitsis; C. R. I. Clayton
π
Article
π
2008
π
John Wiley and Sons
π
English
β 166 KB
## Abstract Unless effective corrections can be applied, satellite remote sensing data will remain modified by the absorption and scattering effects of the atmosphere through which the electromagnetic radiation must pass, between the Sun, the ground and the sensor. The true reflectance of the land