quantifying aerosol types and their impact on trace gas retrievals from satellite measurements
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Vijay Natraj (California Institute of Technology) Hartmut Bösch (Jet Propulsion Laboratory) Yuk Yung (California Institute of Technology). Quantifying Aerosol Types and Their Impact on Trace Gas Retrievals From Satellite Measurements. - PowerPoint PPT PresentationTRANSCRIPT
AGU Fall Meeting December 4, 2005
Vijay Natraj (California Institute of Technology) Vijay Natraj (California Institute of Technology) Hartmut Bösch (Jet Propulsion Laboratory)Hartmut Bösch (Jet Propulsion Laboratory)
Yuk Yung (California Institute of Technology)Yuk Yung (California Institute of Technology)
Quantifying Aerosol Types and Their Quantifying Aerosol Types and Their Impact on Trace Gas Retrievals From Impact on Trace Gas Retrievals From
Satellite MeasurementsSatellite Measurements
AGU Fall Meeting December 4, 2005
Major Source of Retrieval UncertaintyMajor Source of Retrieval Uncertainty
Ground surface
Aerosol Layer 1
Aerosol Layer 2
Light reaching
the detector
Photon path length is enhanced
through multiple scattering by
aerosols
Incident light
AGU Fall Meeting December 4, 2005
Global Aerosol ClimatologyGlobal Aerosol Climatology
Courtesy: Kahn et al, 2001
AGU Fall Meeting December 4, 2005
Aerosol Optical PropertiesAerosol Optical Properties
• Each mixing group is a combination of 4 different aerosol components from a basic set of 7 (Kahn et al., 2001).
• Sulfate (land/water), seasalt, carbonaceous, black carbon: spherical => Mie code (de Rooij and van der Stap, 1984)
• Mineral dust (accumulated/coarse): mixture of oblate and prolate spheroids => T-matrix code (Mishchenko and Travis, 1998)
• Lognormal distribution
• Polarization fully considered
AGU Fall Meeting December 4, 2005
Scattering Matrix (755 nm)Scattering Matrix (755 nm)
AGU Fall Meeting December 4, 2005
Forward Model DetailsForward Model Details
• Park Falls, Wisconsin, July (SZA = 31 degrees)
• Exponential drop-off in aerosol extinction (scale height: ~ 1 km, optical depth: 0.1)
• OCO spectral regions
• Forward model: RADIANT (Christi, CSU) + single scattering approximation for polarization
• Lorentzian instrument lineshape function (resolving powers: O2 A band: 17000, CO2 bands: 20000)
AGU Fall Meeting December 4, 2005
Weighting Functions (OWeighting Functions (O22 AA Band) Band)
0.758 0.760 0.762 0.764 0.766 0.768 0.770 0.772-10
-8
-6
-4
-2
0
2
4
6
8
No
rma
lize
d J
aco
bia
n
Wavelength [m]
Type 1a 1b 1c 2a 2b 3a 3b 4a 4b 4c 5a 5b 5c
AGU Fall Meeting December 4, 2005
Weighting Functions (Weak COWeighting Functions (Weak CO22 Band) Band)
1.590 1.595 1.600 1.605 1.610 1.615 1.620
-0.4
-0.2
0.0
0.2
0.4 Type 1a 1b 1c 2a 2b 3a 3b 4a 4b 4c 5a 5b 5c
No
rma
lize
d J
aco
bia
n
Wavelength [m]
AGU Fall Meeting December 4, 2005
Weighting Functions (Strong COWeighting Functions (Strong CO22 Band) Band)
2.04 2.05 2.06 2.07 2.08
-0.10
-0.05
0.00
0.05
0.10
No
rma
lize
d J
aco
bia
n
Type 1a 1b 1c 2a 2b 3a 3b 4a 4b 4c 5a 5b 5c
Wavelength [m]
AGU Fall Meeting December 4, 2005
Retrieval Groups: Single Scattering AlbedoRetrieval Groups: Single Scattering Albedo
0.755 0.785 1.56 1.65 2.03 2.090.80
0.85
0.90
0.95
1.00
0.755 0.785 1.56 1.65 2.03 2.090.80
0.85
0.90
0.95
1.00
0.755 0.785 1.56 1.65 2.03 2.090.80
0.85
0.90
0.95
1.00
0.755 0.785 1.56 1.65 2.03 2.090.80
0.85
0.90
0.95
1.00
0.755 0.785 1.56 1.65 2.03 2.090.80
0.85
0.90
0.95
1.00
Type 5b
Wavelength [m]
Sin
gle
Sca
tter
ing
Alb
edo
Group 4Type
3b
Group 5
Type 2b 4b 4c
Sin
gle
Sca
tter
ing
Alb
edo
Group 2
Type 3a 5a 5c
Group 3
Type 1a 1b 1c 2a 4a
Sin
gle
Sca
tter
ing
Alb
edo
Group 1
AGU Fall Meeting December 4, 2005
Retrieval Groups: Normalized Extinction CoefficientRetrieval Groups: Normalized Extinction Coefficient
0.755 0.785 1.56 1.65 2.03 2.090.10.20.30.40.50.60.70.80.91.01.1
0.755 0.785 1.56 1.65 2.03 2.090.10.20.30.40.50.60.70.80.91.01.1
0.755 0.785 1.56 1.65 2.03 2.090.10.20.30.40.50.60.70.80.91.01.1
0.755 0.785 1.56 1.65 2.03 2.090.10.20.30.40.50.60.70.80.91.01.1
0.755 0.785 1.56 1.65 2.03 2.090.10.20.30.40.50.60.70.80.91.01.1
Nor
mal
ized
Ext
inct
ion
Coe
ffici
ent
Type 5b
Wavelength [m]
Group 4
Type 3b
Group 5
Type 2b 4b 4c
Nor
mal
ized
Ext
inct
ion
Coe
ffic
ient Group 2
Type 3a 5a 5c
Group 3
Nor
mal
ized
Ext
inct
ion
Coe
ffici
ent
Type 1a 1b 1c 2a 4a
Group 1
AGU Fall Meeting December 4, 2005
Sensitivity TestsSensitivity Tests
• Measurement error: 0.43 ppm
• Smoothing error: 0.29 ppm
• Error due to incorrect assumption of aerosol type within retrieval group
– Group 1: 0.27 ppm
– Group 2: 0.02 ppm
– Group 3: 0.03 ppm
AGU Fall Meeting December 4, 2005
ConclusionsConclusions
• Aerosol retrieval groups determined from basic aerosol mixing groups
• Choosing incorrect mixing group within retrieval group leads to small errors
• Need to test more scattering geometries to validate retrieval types
• More realistic aerosol profiles need to be included
AGU Fall Meeting December 4, 2005
AcknowledgmentsAcknowledgments
• OCO L2 Team (JPL)
• Matt Christi (CSU)
• Michael Mishchenko (GISS)
• Olga Kalashnikova and Ralph Kahn (JPL)
AGU Fall Meeting December 4, 2005
Related Talks/PostersRelated Talks/Posters
• Charles Miller (A14C-02)
• Hartmut Boesch (A12D-05)
• Gretchen Aleks (A33B-0883)
AGU Fall Meeting December 4, 2005
• Need to consider both atmospheric/surface and instrumental polarization
Importance of PolarizationImportance of Polarization