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Global Measurements of Pollution from Space - The MOPITT Experiment. James R. Drummond, Department of Physics, University of Toronto [email protected] Tel: 416-978-4723. Institute of Environmental Physics and Remote Sensing University of Bremen – 23 October 2001. - PowerPoint PPT Presentation
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Global Measurements of Global Measurements of Pollution from Space - The Pollution from Space - The
MOPITT ExperimentMOPITT Experiment
James R. Drummond, Department of Physics,
University of [email protected] Tel: 416-978-4723
Institute of Environmental Physics and Remote Institute of Environmental Physics and Remote SensingSensing
University of Bremen – 23 October 2001University of Bremen – 23 October 2001
23 October 2001 JRD - Bremen
MOPITT Team• AGENCIES• University of Toronto• York University• University of Saskatchewan• McGill University• National Center for Atmospheric
Research (NCAR)• Oxford University• Canadian Space Agency (CSA)• Meteorological Service of Canada
(MSC)• North Carolina State University
(NCSU)• COM DEV International• Hughes-Leitz• BOMEM• SED• NSERC• NASA
• Principal Investigator– James R. Drummond
• Co-Investigators– G.P. Brasseur, Max-Plank– G.R. Davis,
Saskatchewan– J.C. Gille, NCAR– G. Mand, Toronto– J.C. McConnell, York– G.D. Peskett, Oxford, UK– H.G. Reichle, Jr., NCSU– N. Roulet, McGill– J. Wang, SPIE
http://www.atmosp.physics.utoronto.ca/mopitt/home.htmlhttp://www.eos.ucar.edu/mopitt/home.html
23 October 2001 JRD - Bremen
MOPITT
• Introduction• How it all works• How we put it together• Events of the last 600 days• Some successes (it’s working well..)
23 October 2001 JRD - Bremen
23 October 2001 JRD - Bremen
MOPITT
• MOPITT measures gas concentrations in the troposphere (0-15km)
• A very challenging region because of– Underlying surface– Heterogeneous structure– Clouds
23 October 2001 JRD - Bremen
MOPITT
• The troposphere couples to the surface and to biological processes
• Region of the atmosphere most prone to modification, natural or induced
• MOPITT is making global measurements of:– Carbon monoxide profiles– Methane column amounts
23 October 2001 JRD - Bremen
The MAPS Experiment• The MAPS instrument
on the shuttle showed some of the features of the global CO field.
• Outflow from biomass burning events can be seen in this map. Other features can be seen in other seasons.
• But… incomplete...
23 October 2001 JRD - Bremen
Tropospheric Chemistry• The lifetime of CO
(about a month) means it is moved by the dynamics
• Studies of tropospheric chemical transport
• CO is also involved in tropospheric chemistry.
• It interacts with OH and O3
23 October 2001 JRD - Bremen
The Methane Problem• Methane is a greenhouse
gas and a chemical agent.
• Most measurements of methane have been made from the ground (e.g.this picture)
• Considerable debate about the methane budget (sources/sinks) and possible climatic and anthropogenic influences
23 October 2001 JRD - Bremen
MOPITT MeasurementsParameterMeasured
COprofile
COcolumn
CH4
column
Spectral Range 4.7µm 2.4µm 2.3µm
Altitude Range(km)
0-15 - -
VerticalResolution (km)
3-4 - -
HorizontalResolution (km)
22 x 22 22 x 22 22 x 22
TemporalResolution (secs)
0.4 0.4 0.4
EstimatedPrecision
10% 10% 1%
23 October 2001 JRD - Bremen
Measurement Scenario
• MOPITT operates by sensing infra-red radiation from either:
• The surface thermal emission at 4.7µm for CO profiles
• Reflected sunlight at about 2.2-2.4µm for CO and CH4 column measurements in daylight
– The radiation is modified by absorption/emission processes in the atmosphere and these changes are detected in the MOPITT instrument using Correlation Radiometry (CR) techniques
23 October 2001 JRD - Bremen
Correlation Radiometry
• Correlation Radiometry (CR) Uses a sample of the gas of interest as a filter to separate out the required emissions from the background.
• It has been used on a number of spacecraft instruments.
• MOPITT uses two methods of CR– Pressure modulation using Pressure Modulator Cells
(PMCs)– Length modulation using Length Modulator Cells
(LMCs)
23 October 2001 JRD - Bremen
Simple CR System
23 October 2001 JRD - Bremen
• In a CR system the amount of the gas is modulated and the incoming radiation is passed through the gas cell.– Radiation is modulated at the cell
frequency if it's optical frequency coincides with that of a spectral line of the gas in the cell.
– Detection of the modulated part of the radiation is performed digitally and this is a better indicator of the spectrum of interest than the raw radiance.
– Advantages are the reduction of required dynamic range and rejection of other gaseous emission
– Disadvantage is the complexity of the resulting signal
23 October 2001 JRD - Bremen
Wavelength Regions• CO fundamental band at
4.7um – Gives information on profile– But no sensitivity at ground
• CO overtone at 2.3um– Sensitive to column– Only works in sunlight
• CH4 at 2.2um– Same as CO overtone– Quite weak
23 October 2001 JRD - Bremen
Atmospheric Spectrum
3.0
2.5
2.0
1.5
1.0
0.5
0.0
TO
A R
ad
ian
ce
(x
10-3
) [
W/(
m2 s
r c
m-1
)]
222022002180216021402120
Wavenumber (cm-1)
1.0
0.8
0.6
0.4
0.2
0.0
Tra
ns
mitta
nc
e
N2O band
23 October 2001 JRD - Bremen
23 October 2001 JRD - Bremen
MOPITT - Technology
• Uses cooled detectors
• cooled preamplifiers• cooled optics• Active cooling• Digital Signal
Processing• Length Modulators• Pressure Modulators
23 October 2001 JRD - Bremen
• LMCs are the two circular object
• LMCs are made of Ti• Windows are coated
Ge• “Gold” object is a
molecular sieve
23 October 2001 JRD - Bremen
MOPITT - Instrument
23 October 2001 JRD - Bremen
MOPITT Calibration
• MOPITT has a saw-tooth scan - takes 13 secs
• A space view is taken every 10 scans• A two-point calibration is taken every 11
minutes• A long calibration is performed monthly.
23 October 2001 JRD - Bremen
MOPITT - Scanning
23 October 2001 JRD - Bremen
MOPITT - Vertical Resolution
23 October 2001 JRD - Bremen
MOPITT - Instrument
23 October 2001 JRD - Bremen
Terra Spacecraft
23 October 2001 JRD - Bremen
Terra - Other Instruments• ASTER - ASTER - Advanced Spaceborne Thermal Emission and Reflection Advanced Spaceborne Thermal Emission and Reflection
RadiometerRadiometer – 15m resolution, 0.5-12um15m resolution, 0.5-12um– Surface ImagerSurface Imager
• MISR - MISR - Multi-angle Imaging SpectroRadiometerMulti-angle Imaging SpectroRadiometer– 9 cameras, 275m resolution 0.44 - .87um9 cameras, 275m resolution 0.44 - .87um– Multi-angle surface imagerMulti-angle surface imager
• MODIS - MODIS - Moderate Resolution Imaging SpectrometerModerate Resolution Imaging Spectrometer– 250m resolution 0.4-14.5um250m resolution 0.4-14.5um– Surface imagerSurface imager
• CERES - CERES - Clouds and the Earth’s Radiant Energy SystemClouds and the Earth’s Radiant Energy System– 10km resolution, 0.3-50um10km resolution, 0.3-50um– Global radiation budgetGlobal radiation budget
23 October 2001 JRD - Bremen
LAUNCH!!
• Failed launch attempt– December 16, 1999– Change of procedure
• Successful launch– Dec 18, 1999, 18:57GMT
(10:57PST)– 9 seconds before end of window!
• Orbit:– polar, sun synchronous, – Altitude, 705km, inclination 98.4– 10:43am desc. node
23 October 2001 JRD - Bremen
23 October 2001 JRD - Bremen
23 October 2001 JRD - Bremen
The First Map!
23 October 2001 JRD - Bremen
Instrument Maintenance
• MOPITT is mostly self-calibrating– Thermal (longer wavelength) channels calibrate
• every 2 minutes to space• Every 11 minutes to internal (room temperature) target
– Solar (shorter wavelength) channels calibrate• Every 2 minutes to space• Every 11 minutes to internal (room temperature) target• Every few months to internal (hot – 450K) target
– Cold systems need monitoring– Gas cells need attention….
23 October 2001 JRD - Bremen
On-Orbit Gain Trend• Icing on the cold optics
leads to a change in transmission and hence a gain change
• Thermal channels– Initial rate of change 1%/21
days– 2nd de-contamination
brought gain values to within 1% of initial values
– Present rate is 1%/60 days
• Solar channels– Initial rate of change
1%/100 days– 2nd de-contamination
brought gain values to within 0.5% of initial values
– Present rate is 1%/120 days
0.94
0.95
0.96
0.97
0.98
0.99
1
1.01
Norm
alised G
ain
50 100 150 200 250 300 350
Ops day (MET-13 days)
Ch 1 Ch 3 Ch 7 Ch 2 Ch 8 Ch 4
•De-contamination criteria in the future may depend on a filter shift criteria rather than a gain change
23 October 2001 JRD - Bremen
MAPS
• Before • After
23 October 2001 JRD - Bremen
One Day of MOPITT Data
23 October 2001 JRD - Bremen
Map average global may
23 October 2001 JRD - Bremen
Map average global october
23 October 2001 JRD - Bremen
Map average NA may
23 October 2001 JRD - Bremen
Map average NA october
23 October 2001 JRD - Bremen
MOPITT – THE MOVIES - I
23 October 2001 JRD - Bremen
MOPITT – THE MOVIES - II
23 October 2001 JRD - Bremen
China Weather and China Weather and MOPITTMOPITTCO for 22CO for 22ndnd August August 20002000
-MOPITT data are not available under hurricane “BIBILIS”
- Transition from high CO to low CO visible across the front
23 October 2001 JRD - Bremen
MOPITT - Validation Strategy
• Pre-launch algorithm test and verification– Use aircraft data– Add to spectral database
• Validation of MOPITT level 1 data:– Comparison with model calculations– MOPITT airborne simulator (MOPITT-A)– MOPITT Algorithm Test Radiometer - MATR – FTIR Measurements– MODIS/MAS.
• Comparison of derived products (mainly level 2 data) with correlative measurements.– Ground-based spectroscopy– Airborne in situ measurements– ground-based in situ measurements at selected sites
•
23 October 2001 JRD - Bremen
0 61 122 183 244 305 366 427 488 549
0
100
200
CO
mix
ing
ra
tio
, p
pb
v
Days after January 1, 2000
Circles: ground-based spectrometer (column)Open Triangles: MOPITT 850hPaSolid Triangles: MOPITT, middle & upper troposphere
23 October 2001 JRD - Bremen
MOPITT Anomalies
• MOPITT has been operational at 100% since March 2000• The first event occurred on May 7th 2001 (OPS127/04:07:00)• The telemetry indicated that displacer B amplitude was
excessive– Triggered Red Limit– MOPITT to SAFE as per pre-arranged procedure– Red condition occurred for about 11 minutes before SAFE mode
• Subsequent analysis indicated that during the 11 minutes– Tip B temperature increased at a rate higher than if coolers had
been turned off– Compressors A and B increased amplitude– Tip A cooled down
23 October 2001 JRD - Bremen
MOPITT OPTICS
Cooler B
Cooler A
23 October 2001 JRD - Bremen
MOPITT Anomalies
• July 5th onwards• MOPITT in SCIENCE mode• Operating normally on channels 5-8 only• Channels 1-4 are off with detectors unpowered and tip
at slightly above room temperature.• Long calibration was initiated to retrieve calibration
baseline• Cooler sub-system exhibiting more amplitude wander
than previously observed, but this is not impacting operations
23 October 2001 JRD - Bremen
23 October 2001 JRD - Bremen
MOPITT Anomalies
• On August 7 Chopper 3 motor drive current fell to zero– Not a flagged condition– no danger to instrument
• Subsequent investigation showed that power feed to the chopper had failed at (nearly) the same time
• Some indications of high current draw in the few seconds before failure
• No indication in previous telemetry of any problem• Symptoms are exactly the same as for an unverified
fuse failure pre-launch
23 October 2001 JRD - Bremen
MOPITT Anomalies
• Channels 5 and 6 are affected• Analysis of science telemetry indicates that the chopper
has failed completely open• Chopper is “loose” in the instrument
– Maneuvers in the roll direction are the most likely to cause the chopper to close
• Algorithms are being developed to utilise Channel 5 and Channel 6 data without the chopper closed information
• Initial indications are that this might be successful• Space view is being used as a substitute for the chopper
closed• Some instrument optimisation results in improved signals
23 October 2001 JRD - Bremen
23 October 2001 JRD - Bremen
Current Status
• 14 months of fully operational instrument• Data are being successfully processed for full
instrument and in current restricted mode• Data are now available at Langley DAAC• Validation is underway• There is still a lot of work to do….• There is some discussion of a MOPITT follow-
on