Py. Deschamps et al., THE POLDER MISSION - INSTRUMENT CHARACTERISTICS AND SCIENTIFIC OBJECTIVES, IEEE transactions on geoscience and remote sensing, 32(3), 1994, pp. 598-615
This paper introduces the new Polarization and Directionality of the E
arth's Reflectances (POLDER) instrument. The spaceborne POLDER sensor,
which is selected to fly aboard the Japanese ADEOS satellite schedule
d for launch in early 1996, has nearly complete phase C of its develop
ment at the Centre National d'Etudes Spatiales, the French space agenc
y. To prepare for the 1996 space mission, airborne prototypes are bein
g tested and evaluated in the framework of various measurement campaig
ns. The POLDER sensor is designed to collect global observations of po
larized and directional solar radiation reflected by the Earth-atmosph
ere system for climate and global change studies. Aboard the ADEOS pla
tform, the POLDER mission will provide near-daily coverage of the Eart
h at 6 x 7 km2 resolution. The POLDER system will offer unprecedented
opportunities to observe biophysical parameters over the oceans and la
nd surfaces. The sensor's unique features, when compared to current an
d planned spaceborne instruments, include its ability to: 1) measure p
olarized reflectance in the visible and near-infrared spectral regions
; 2) observe Earth target reflectance from 12 directions during a sing
le satellite pass; and 3) operate in two dynamic modes in order o achi
eve both high signal to noise ratio and wide dynamic range. Six of POL
DER's eight channels are optimized for observing a atmospheric aerosol
s, clouds, ocean color, and land surfaces. The other two are centered
on the H20 and 02 absorption bands for retrieving atmospheric water va
por amount and cloud top altitude, respectively. POLDER data will be s
ubject to the high calibration standards defined by the POLDER mission
team, with absolute calibration accuracies of 2% for the shorter wave
length channels (lambda less-than-or-equal-to 565 nm) and 3% for the l
onger wavelengths. A 1% accuracy is the goal for the intercalibration
between the spectral channels. The POLDER instrument aboard ADEOS will
contribute significantly to climate-related research on aerosol cycli
ng, cloud-radiation interactions, the Earth radiation budget, ocean pr
imary productivity, and continental biosphere dynamics. Using POLDER c
apability to measure bidirectional reflectance and polarization distri
bution in functions for estimating biophysical parameters, the POLDER
mission's scientific objectives will be to: 1) map atmospheric aerosol
s, including their sources and transport, and study their influence on
the Earth radiation budget; 2) assess cloud properties, namely their
height, phase and type; 3) estimate total integrated water vapor amoun
t; 4) improve Earth radiation budget estimates; 5) estimate chlorophyl
l-like pigment content in the ocean surface layer and its role in the
carbon cycle; and 6) characterize land surface properties and vegetati
on cover. In meeting these objectives, POLDER will play an important r
ole in advancing the measurement and research objectives of the World
Climate Research Program (WCRP) and the International Geosphere and Bi
osphere Program (IGBP).