Results of POLDER in-flight calibration

Citation
O. Hagolle et al., Results of POLDER in-flight calibration, IEEE GEOSCI, 37(3), 1999, pp. 1550-1566
Citations number
41
Categorie Soggetti
Eletrical & Eletronics Engineeing
Journal title
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING
ISSN journal
01962892 → ACNP
Volume
37
Issue
3
Year of publication
1999
Part
2
Pages
1550 - 1566
Database
ISI
SICI code
0196-2892(199905)37:3<1550:ROPIC>2.0.ZU;2-7
Abstract
POLDER is a CNES instrument on board NASDA's ADEOS polar orbiting satellite , which was Successfully launched in August 1996, On October 30, 1996, POLD ER entered its nominal acquisition phase and worked perfectly until ADEOS's early end of service on June 30, 1997, POLDER is a multispectral imaging r adiometer/polarimeter designed to collect global and repetitive observation s of the solar radiation reflected by the earth/atmosphere system, with a w ide field of view (2400 km) and a moderate geometric resolution (6 km), The instrument concept is based on telecentric optics, on a rotating wheel car rying 15 spectral filters and polarizers, and on a bidimensional charge cou pled device (CCD) detector array. In addition to the classical measurement and mapping characteristics of a narrow-band imaging radiometer, POLDER has a unique ability to measure polarized reflectances using three polarizers (for three of its eight spectral bands, 443 to 910 nm) and to observe targe t reflectances from 13 different viewing directions during a single satelli te pass. One of POLDER's original features is that its in-flight radiometric calibra tion does not rely on any on-board device. Many calibration methods using w ell-characterized calibration targets have been developed to achieve a very high calibration accuracy. This paper presents the various methods impleme nted in the in-flight calibration plan and the results obtained during the instrument calibration phase: absolute calibration over molecular scatterin g, interband calibration over sunglint and clouds, multiangular calibration over deserts and clouds, intercalibration with Ocean Color and Temperature Scanner (OCTS), and water vapor channels calibration over sunglint using m eteorological analysis. A brief description of the algorithm and of the per formances of each method is given.