jem/smiles が拓く地球大気観測 - 大阪府立大学 宇宙物 · pdf...
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JEM/SMILES が拓く地球大気観測
笠井康子(NICT)JEM/SMILES Mission Team (NICT & JAXA)
NICT: National Institute of Information and Communications TechnologyJAXA: Japan Aerospace Explosion Agency
第10回 受信機ワークショップ「ミリ波サブミリ波受信機ワークショップ」5 March , 2010
SUBMILLIMETER-WAVE LIMB-EMISSION SOUNDER (SMILES)
There are two target for SMILES Mission1. Space demonstration of the super-conductive submillimeter-wave technology, 4K mixer and its mechanical cooler. 2. Demonstration of 4K super sensitive atmospheric observation with submillimeter-wave limb-emission sounding.
JEM/SMILES MissionSuperconducting Submillimeter-Wave Limb-Emission Sounder (SMILES) designed to be aboard the Japanese Experiment Module (JEM) on International Space Station (ISS)Collaboration project of NICT and JAXA NICT: National Institute of Information and Communications Technology. JAXA: Japan Aerospace Exploration Agency
Scientific Targets of SMILES
1. Ozone recovery (Stratosphere):Sensitive observation of Ozone, HCl, ClO HOCl, HO2, H2O2, BrO, and HOBr etc will contribute to understand the recent status of ozone layer in mid-latitude region.
2. Climate change (UT/ LS):Sensitive Observation of Humidity, Ice cloud, HCl isotopes, Ozone isotopes, and CH3CN in UT/LS region with solar zenith angle dependence. UT/LS atmospheric exchange, diurnal variation of heterogeneous reaction on ice cloud.
3. First observation (Mesopause):First global day and night continuous sensitive observation of
atmospheric compositions, O3, HCl, HO2, in the mesopause.
SMILES sensor and observation method
Observation Freq. (GHz)
BandA: 624.32-625.52BandB: 625.12-626.32BandC: 649.12-650.32
Antenna FOVReceiverSpectrometer
0.009(HPBW)SIS mixer+ HEMT ampAOS
Resolution 1.8 MHz Tsys 500K expected -> 300K real
Integ. time 0.5 sec/spectrum Geometry Limb scanning
Orbit Non- sun synchronized orbit (allow to observe diurnal variation within 24 hours)
Scan Altitude -30km to 120km
4K mechanical cooler
SIS mixer: 4K Super-conductive receiver
InputOptics
20K
HEMTAmp
SISMixer
Cryostat
Mechanical CoolerSub-mm
LO
AOS9-15GHz
IF
638.5 GHz
Antenna
Development of Microwave Limb Emission Sounder
UARS/MLS was the first satellite mission for “Microwave Limb Sounder”. Odin/SMR is the first “Sub-millimeter-wave sensor”. JEM/SMILES is the first “super-conductive sensor”.
Aura/MLSTsys: 12000K(DSB@650GHz)
Odin/SMRTsys: 3000K(SSB@500GHz)
UARS/MLS JEM/SMILESTsys: 300K(SSB@650GHz)
1991 20042001 2009
Aura/MLSTsys: 12000K(DSB@650GHz)
Odin/SMRTsys: 3000K(SSB@500GHz)
JEM/SMILESTsys: 300K(SSB@650GHz)
Simulated spectrum with several noise corresponding with MLS, Odin/SMR, and SMILES. For comparison, SMILES instrumental setup are used for all simulations. This is “NOT” the simulation of MLS and Odin/SMR observation .
Comparison of spectrum noise
ClO
HO2
6000K 3000K 300K
s=6K s=0.3K
Averaging kernel
black-dots: a priori errorfull line: single scan precisiondashed line: daily average precisiondash-dot line: monthly average
Averaging kernel of SMILES O3 : Observe 10-90kmまで観測可能
Averaging kernel Averaging kernel
Data transfer
L3 data
L0/L1b data
L2 OperationalSteady, Real time, and Complete system for operational processing
JAXA/TKSC
NICT
NICT
JAXA/ISAS
L2 ResearchFlexible, Fast, and Small systemfor research processing
NASA/USA
ISS
L2r processing
Algorithm development
Spectroscopic study
JAXA (Tsukuba)level 0,HK, 1b
L2 L3L1
System/job management
JAXA/ ISAS L2 operational
Database/ File storage
Data dow
nload services
NASA GODDARD Meteorological data
System Over View
Data backup
L3 processing
ValidationACE(tele-con 1/week)MLSOdin/SMR OSIRIS SCIAMACHY
L3 QLData distribution
other data …
System model of SMILES retrieval algorithm
Synthetic radianceObserved radiance
<L1b products>Atmospheric State
<Nature>
Retrieval State<L2 products>
Forward calculationRadiative Transfer
Sensor model
Retrieval Analysis
Error Analysis
Observed Spectrum
Forward calculationRadiative Transfer
Sensor model
R
Atmospheric radiation
Key components are:1. Antenna: Antenna Pattern2. SSB filter: Side band ratio3. AOS spectrometer: Response function
These components “were” measured and parameterized by the instrument team before launch!
Observed Spectrum
Almost no standing wave on the spectrum!Stable spectrum over day!
Temperature control system on JEM/ISS was quite good
Great things:- Less noise than expected. 500K -> 300K- NO standing wave on the spectrum.- Stable less than 1K over scan.
Problems (as S. Ochiai said):- Pointing problem: Bad pointing information with no oxygen observation. Both ISS and Star Tracker has different problem.
- No linearity problem of the spectrum:
System model of SMILES retrieval algorithm
Forward calculation
Synthetic radianceObserved radiance
<L1b products>Atmospheric State
<Nature>
Retrieval State<L2 products>
Radiative Transfer
Sensor model
Retrieval Analysis
Error Analysis
SMILES species
Processing modes
Band A Band B Band C
Stratospheric(major)
O3, H37Cl, H2O,
Temp, Pointing offset
O3, H35Cl, H2O,
Temp, Pointing offset
H2O, ClO
Stratospheric(minor)
wind, HOCl, CH3CN, HNO3, BrO, H2O2, SO2
wind, HO2, HNO3, SO2
O3, HO2, HNO3, BrO
Mesospheric O3, H37Cl, wind,
H2O2
O3, H37Cl, wind,
HO2
HO2, , ClO
UT/LS H2O, Ice water content, O3, CH3CN
A vs C B vs C
A(H37Cl) vs B(H35Cl)A vs B A vs B
O3 @ 30 hPaO3 @ 30 hPa
HCl @ 30 hPa O3 @ 30 hPa Temperature @ 30 hPa
SMILES self-comparisondaily comparison of same products from different bands
30 hPa region: region has relatively smaller non-linear problems in the spectrum S. Ochiai
Early Validation
O3
HCl
ClO
BrO
MLS switch on HCl channel 24-27 Nov.
MLS Odin/SMROSIRIS
ACEGround-based UV/VIS
SCHYAMACHY
Francois Hendrick
Alexei Rozanov
Ozonesonde
SCHYAMACHY
SCHYAMACHY
N. LiveseyB. ReadL. Froidevaux
K. WalkerP. Bernath D. Murtagh
D. Degenstein
Ground-based UV/VIS
MLS/ACE/TELIS/MIPAS-B did measurement of HCl
Ozonesonde
2009/11/13-2009/11/24-bandB-1h400km
25km problem
T.Tanaka, K.Kita, E. Dupuy, Y.Kasai
25km problem
SMILES-Ozonesonde
2009/11/13-2009/11/24-bandB-12h600kmSMILES-MLS
Ozone
M
Jan. 25: SMILES H35Cl/ MLS HClBlack line is averaged values of SMILES, MLS. 466 coincidence (+/- 1hour, +/- 400km)
25km problem
Problem of calibration non-linearity
Difference about 5K
Feedback to S. Ochiai et al., Instrumental team
Difference less than 1K
Early BrO comparison with ground-based DOAS observation
SMILES ('L2product_G_RA' operational product) and ground-based UV-vis BrO profiles over Observatoire de Haute Provence (OHP) in Southern France (44ーN, 5.5ーE).
The coincidence criteria: latitude +/- 5deg, longitude: +/- 10deg.
The ground-based UV-vis BrO profiles have been photochemically corrected in order to correspond to SMILES SZA.
SMILES profiles have been smoothed using ground-based UV-vis averaging kernels.
Ground-based UV/VIS
Francois HendrickBelgian Institute for Space Aeronomy
Decrease of intensity due to scattering from ice particules
dashed line: clear sky
Ice cloud signal on SMILES brightness temperature
An example of early result
SMILES successfully detected diurnal variation of ClO in lower-mid latitude
In one-day data.
ClO daytime ClO night time
Managers: Ryota Sato (JAXA)M. Takayanagi (JAXA)Yasuhiro Murayama (NICT)
PI: Masato Shiotani
SMILES Instrumental Team members:Kikuchi Kenichi (JAXA)Satoshi Ochiai (NICT)Toshiyuki Nishibori (JAXA) Takeshi Manabe (Osaka Pr. U., NICT)Hiroyuki Ozeki (Toho University)
NICT SMILES project members Takahiro Tanaka (Ibaraki University, NICT)Tomohiro Sato (Tokyo Institute of Technology)Eric Dupuy (NICT)
Thanks to colleaguesSMILES Science team members ScienceMakoto Koike (University of Tokyo)Kazuyuki Kita (Ibaraki University)Algorithm developmentPhilippe Baron (NICT)Jana Mendrok (NICT)Donal Murtagh (Chalmers University)Joachim Urban (Chalmers University)Patrick Errikson (Chalmers University)Dong Wu (JPL)Bill Read ( JPL)L2 processing systemMakoto Suzuki (JAXA)Takuki Sano (JAXA)Koji Imai (JAXA)L3 processing systemValidation Tomoo Nagahama (Nagoya Unievrsity)