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PARASOL of CNES Myriade Series
PARASOL (Polarization and Anisotropy of Reflectances for Atmospheric Science coupled with Observations
from a Lidar) is a French (CNES) science mission of the Myriade series, put forward by CNRS/LOA [Laboratoire
d'Optique Atmosphérique at USTL (Lille University of Science and Technology), Lille, France)], with the general
objective to study the Earth's atmosphere. Of particular interest in this study is the role of clouds and aerosols (fine
particles in suspension in the air) in climate mechanisms (which effect has global warming on cloud cover? How do
clouds and aerosols interact?).
The PARASOL mission flies the POLDER-derived instrument as its main payload with the objective to improve
the microphysical and radiative property characterization of clouds and aerosols for model improvement. Clouds
and aerosols play an important role in direct and indirect radiative forcing of the Earth's energy budget. The study
of the dynamic processes and interactions between liquid and solid particles (radiative properties of clouds and
aerosols) in the atmosphere is therefore a major goal. PARASOL (POLDER) complements CALIPSO (Lidar)
and NASA's Aqua and Aura (MODIS, CERES) missions, it also makes use of the CloudSat (CPR) radar data. The
instruments form a so-called "train of satellites," all in the same orbits and in a PM sequence (a loosely-coupled
constellation), provide a unique opportunity of near-simultaneous observations, by collecting data in different
spectral domains (optical and microwave regions) and at various FOVs (Field of Views). 1) 2) 3)
Spacecraft:
The PARASOL microsatellite of CNES
consists of a box-like structure (size: 60 cm x 60 cm x 80 cm) with
deployable solar panels (Myriade microsatellite bus). The S/C is
three-axis stabilized, providing a pointing accuracy of
0.1º, and a knowledge of 0.02º. Attitude sensing is provided
by a star sensor, 3 sun sensors, a magnetometer, and
gyros, actuation is provided by 4 reaction wheels and 3 magnetic
torquers. The solar power is about 180 W (BOL).
The solar array consists of two hinged panels folded against the
platform during launch (array length of 1.7 m, triple
junction AsGa solar cells are used with an efficiency of 26%, providing
180 W of power). The solar array is articulated for maximum power
generation. The Li-ion battery has a capacity of 15 Ah (commercial
product of Sony).
Regulation and distribution of power is provided by PCDU (Power Control
and Distribution Unit). Orbit control
(maintenance) is provided by a blow-down hydrazine system (four 1 N
thrusters, using 4.5 kg of hydrazine, Isp of
210 s). The S/C mass is 120 kg at launch, the mission design life is
one year with two years as goal.
OBC: Centralized onboard data handling is provided by a 10 MIPS T805 microprocessor (a radiation-hardened
transputer at 15 krad). The OBC power consumption is < 6 W with a mass of 3 kg. Serial asynchronous links are
used for onboard data handling.
The PARASOL mission is the second one (after DEMETER) in the Myriade microsatellite series of CNES (see
Myriade overview at end). Myriade also marks the beginning of an innovative partnership between CNES, Alcatel
Space and EADS-Astrium. These two companies helped develop Myriade bus, so they can use the concept for
their own missions.
Spacecraft construction was provided
mainly in-house. CNES also called on its network of industry partners,
including Toulouse-based aero-structures manufacturer
Latécoère to assemble and integrate the microsatellite.
Figure 1: Artist's view of the PARASOL spacecraft (image credit: CNES)
Orbit: Sun-synchronous
circular orbit, altitude = 705 km, inclination = 98.21º, the local
equator crossing time is
at 13:30. PARASOL will be part of the so-called "A-train" consisting of
the Aqua, CloudSat, CALIPSO, PARASOL, and Aura spacecraft.
Note: At the launch of PARASOL, the A-train is consisting of the Aqua (launch 2002) and Aura (launch 2004)
spacecraft of NASA. CALIPSO and CloudSat are going to follow in 2005. In addition, the OCO (Orbital Carbon
Observatory) minisatellite of NASA was assigned to the A-train, with a planned launch in 2007/8.
Launch: A launch of PARASOL as a secondary payload on Ariane-5G+ from Kourou took place on Dec. 18,
2004. Another secondary payload was NanoSat1 of INTA, Spain.
The primary payloads on this flight
were Helios-2A (launch mass of 4200 kg), a military reconnaissance
mission of
DGA, France, in partnership with Spain and Belgium (the first satellite
in France's second-generation military
surveillance system); and four microsatellites called Essaim-1, -2, -3,
and -4. Essaim means `swarm' in French,
they are also of DGA (Délégation Générale
pour l'Armement - French Arms Procurement Agency). The objective is
analysis of the electromagnetic environment (military use). The Essaim
satellites use also the Myriade microsatellite bus of CNES.
Figure 2: Illustration of the A-train constellation (image credit: CNES)
Figure 3: Illustration of the A-train observations (image credit: NASA)
Communications: A payload mass memory provides a capacity of 16 Gbit. RF communications are provided in
S-band (frequency = 2.2 GHz) at a downlink data rate of 400 kbit/s and an uplink rate of 20 kbit/s. In addition,
there is an X-band downlink for payload data (8 GHz, 16.8 Mbit/s data rate) with a modulation scheme in QPSK.
The communication protocol is in CCSDS standard.
Mission status: The PARASOL spacecraft is operating nominally as of 2008. 4)
• The PARASOL spacecraft
reached its final 705 km orbit in March 2005 and joined the A-train of
NASA flying with Aqua, CALIPSO, CloudSat, and Aura).
• As of April 2005, the
spacecraft and its instruments completed the commissioning phase.
Important maneuvers were conducted during the commissioning phase to
get into the final operational orbital slot (SSO, 705 km
altitude, LTAN of 13:30 hours). Now, the PARASOL orbit control imposes
to keep the S/C in a prescribed "box".
The needed maneuvers are being conducted nearly each month - with the
consequence that each time the scientific mission is "off" for two
orbits.
• As of fall 2005, PARASOL was set to begin its mission to observe clouds and aerosols in the A-train.
• As of fall 2005, the hydrazine left in the propulsion system is sufficient to maintain station keeping for > 10
years.
• On-orbit operational lessons learnt: The DEMETER operational experience and feedback has permitted to
upload corrections on the PARASOL platform software very soon after its launch (both S/C are of the same family).
Sensor complement:
POLDER-P (Polarization and
Directionality of the Earth's Reflectances - PARASOL), a CNES
instrument (radiometer/polarimeter) of ADEOS and ADEOS-II mission
heritage. POLDER-P is an improved version of
POLDER1/2, designed at the LOA atmospheric optics laboratory in Lille
(CNRS-USTL) and built by EADS-Sodern. The objective is the measurement
of multidirectional and polarized solar VIS/NIR radiation reflected by
the atmosphere and Earth's surface, and aerosols. POLDER-P consists
basically of a digital staring camera composed of a 274 x 242 pixels
CCD detection array, wide field-of-view telecentric optics (±
51º cross-track and ±
43º along-track) and of a rotating wheel carrying spectral and
polarized filters. 5) 6) 7) 8)
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Instrument mass, volume
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32 kg, 0.8 m x 0.5 m x 0.25 m
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Power consumption
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50 W (image mode)
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Data quantization, data rate
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12 bit, 883 kbit/s
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FOV (Field of View)
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± 43º along track; ± 51º cross track
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Swath width
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2400 km
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Ground resolution (at nadir)
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6 km x 7 km
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Table 1: POLDER-P instrument parameters
Figure 4: Illustration of the PARASOL payload (image credit: CNES)
The
sensor concept is based upon the application of polarization filters
and measures in a number of spectral bands
and at various observation angles (multiangle viewing capability).
Compared to POLDER-1/2, the telecentric
optics array has been turned 90º to favor multidirectional viewing
over daily global coverage. Likewise, a 1020 nm
waveband has been added to conduct observations for comparison with
data acquired by the lidar on the CALIPSO mission, one of its companion
satellites on the A-train. POLDER-P also relies on the innovative
techniques
developed to calibrate the POLDER1/2 instruments, using in particular
the sun's reflection from the ocean surface, clouds and desert areas as
targets to validate inflight performance.
A motorized filter wheel enables the successive study of different wavebands of visible light. By adding a band in
the near-infrared, POLDER-P expands the spectrum being analyzed, and provides an even richer harvest of
scientific data.
POLDER has nine spectral channels,
three of which are implemented with polarized filters (total of 15
channels,
three channels are needed for each polarized band). The spectral region
is from 443 to 910 nm. For the polarized
wavelengths, 3 filters measure the linear polarization of the incoming
radiation in three directions separated by
120º. The observed data permit the derivation of the Stokes
parameters and the total irradiance. The acquisition of
an image sequence takes 20 seconds, enabling the observation of one
natural target from different directions. The
radiometric performances of POLDER-P are similar to those of POLDER-1/2
flown on ADEOS and
ADEOS-II, respectively. The vicarious calibration methods, based on the
observation of natural targets (no calibration system on board
PARASOL), are also the same as those of the POLDER-1/2 instruments.
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POLDER-1/2
channels
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Bandwidth
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POLDER-P channels (band
center)
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Comments/observations
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Saturation level
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443P nm
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20 nm
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444.5 P nm
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Polarization moved to 490 nm
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1.1
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443 nm
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20 nm
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444.9 NP nm (highly dynamic
range)
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Cloud detection, drop of ocean color
applications
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0.97
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490 nm
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20 nm
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492.2 nm (addition of
polarization)
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Aerosol retrieval, cloud pressure
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0.75
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565 nm
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20 nm
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564.5 nm (highly dynamic
range)
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Lidar at 532 nm
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0.48
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670P nm
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20 nm
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670.2 P nm (no change)
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Aerosol retrieval, cloud properties
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1.1
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865P nm
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40 nm
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860.8 P nm
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Aerosol retrieval, cloud properties
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1.1
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763 nm
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10 nm
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763.3 nm
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Cloud oxygen pressure by differential
absorption technique in Oxygen A band
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1.1
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765 nm
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40 nm
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763.1 nm
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1.1
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910 nm
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20 nm
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907.3 nm
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Water vapor retrieval
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1.1
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Table 2: Spectral bands of POLDER (comparison of bands with heritage instruments)
The saturation levels are given in units of normalized radiance, i.e., the maximum spectral radiance divided by the
solar spectral radiance at nadir and multiplied by π. The dynamic reflectance range is subsequently obtained by
dividing the range by cos θs, where θs is the solar zenith angle.
A scene (a 2D image) has a size of about 1600 km (along-track) x 2400 km (cross-track) with a ground spatial
resolution of 6 km x 7 km at nadir.
Instrument accommodation: POLDER-P has a mass of about 32 kg, a size of about 80 cm x 50 cm x 25 cm, the
power consumption = 50 W in imaging mode (mean power of 29 W). The data rate is 883 kbit/s at 12 bit quantization.
Figure 5: Cut-away view of the POLDER-P instrument (image credit: ICARE)
Figure 6: Overview of POLDER-P instrument filter settings (image credit: CNES)
Figure 7: POLDER-P instrument response (image credit: ICARE)
Ground segment:
Mission operations and payload data acquisition are being performed at CNES (Myriade Control Center). The
MIcrosatellite Ground Segment (MIGS) designed by CNES comprises: 9)
• CCC (Command and Control Center) in Toulouse
• Network of S-band (2 GHz) satellite tracking stations
• Two S-band stations at Aussaguel, near Toulouse, and Kiruna in Sweden providing telemetry/telecommand
links
• The TETX (Telemetry Earth Terminal X-band), receiving station in Toulouse for science data reception
• Communication network
• Mission Center in Toulouse
• ICARE Data Processing and Management Center hosted at USTL (Université des Sciences et Techniques de
Lille), Lille, France. Note: ICARE is a research structure set up in 2003 on a national level and consisting of
CNES, INSU, USTL, etc. (all research laboratories) - to study aerosol-cloud-radiation interactions and
the water cycle (cloud properties, atmospheric chemistry) and using data from various missions. 10)
Figure 8: Overview of the MIGS reference architecture, presently with PARASOL and DEMETER (image credit: CNES)
Figure 9: Overview of the PARASOL ground segment (image credit: CNES)
Figure 10: Data products of PARASOL (image credit: CNES)
1) http://smsc.cnes.fr/PARASOL/index.htm
2)
C. Bastien-Thiry, M. Bach, A. Lifermann, "PARASOL a Microsatellite in
the A-Train for Earth Atmospheric Observations," Proceedings of the
5th IAA Symposium on Small Satellites for Earth Observation," April
4-8, 2005, Berlin, Germany
3)
P. Lier, M. Bach, "PARASOL a microsatellite in the A-Train for Earth
atmospheric observations," Proceedings of the 56th IAC 2005, Fukuoda,
Japan, Oct. 17-21, 2005, IAC-05-B5.4.03
4)
C. Bastien Thiry, F. Serene, H. Darnes, F. Duchevet, "DEMETER and
PARASOL after 2 years in orbit: where are we?," Proceedings of the 4S
Symposium: `Small Satellite Systems and Services,' Chia Laguna
Sardinia, Italy, Sept. 25-29, 2006, ESA SP-618
5) "PARASOL - Parasol effect and greenhouse effect," CNES Dossier, Nov. 2004, pp. 20, http://smsc.cnes.fr/PARASOL/dossier_presse_parasol.pdf
6) "Building on the heritage of POLDER and Demeter," http://www.cnes.fr/automne_modules_files/standard/public/p2885_2a1e6c9205cf3ae25c9994e6635d6f6edossier4.pdf
7)
F. Bermudo, B. Fougnie, T. Bret Dibat, "POLDER-2 In-Flight Results and
PARASOL Perspectives," Proceedings of the 5th International Conference
on Space Optics, March 30- April 2, 2004, Toulouse, France, ESA SP-554
8) http://www-icare.univ-lille1.fr/parasol/?rubrique=mission_parasol
9) http://smsc.cnes.fr/MYRIADE/GP_segment_sol.htm
10) http://www-icare.univ-lille1.fr/
This description was provided by Herbert J. Kramer from his documentation of: "Observation of the Earth and Its Environment: Survey of Missions and Sensors" - comments and corrections to this article are welcomed by
the author.
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