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MISR: A Prototype New Product
Michael J. Garay
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
© 2014. All rights reserved.
International Cooperative for Aerosol Prediction (ICAP) 23 October 2014 Boulder, Colorado
Nine view angles at Earth surface: 70.5º forward to 70.5º backward Nine 14-bit pushbroom cameras 275 m - 1.1 km sampling Four spectral bands at each angle: 446, 558, 672, 866 nm 400-km swath: 9-day coverage at equator, 2-day at poles 7 minutes to observe each scene at all nine angles
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Menu
3 3
• Appetizer – About the current MISR product
• Salad – Moving to 4.4 km resolution – NRT?
• Main – The MISR retrieval algorithm
• Dessert – Benford’s Law
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Appetizer
4 4
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Kahn et al. (2010). Multiangle Imaging SpectroRadiometer global aerosol product assessment by comparison with the Aerosol Robotic Network, Journal of Geophysical Research – Atmospheres
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Africa
South America
United States Aug 29 Aug 26 Aug 25 Aug 24 Aug 23 Aug 22 Aug 21 Aug 20 Aug 19
Dust from the Sahara Desert Reaches Houston, Texas
Observations from the Multi-angle Imaging SpectroRadiometer (MISR) Instrument on NASA’s EOS Terra Satellite
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MISR views of Eyjafjallajökull – 4/19/2010
Aerosol particle properties from MISR
7 7
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MISR Version 22 Operational Aerosol Product for July 2007
Key Spherical Non-Absorbing
Spherical Absorbing Non-Spherical 8
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Aerosol climatology from NAVY Aerosol Analysis and Prediction System (NAAPS) for July 2007
Note: AOT < 0.1 not shown 9
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AERONET AOD 550 nm 0 0.2 0.4 0.6 0.8 1
0.2
0.4
0.6
0.8
1
MISR AO
D 550 nm
y = 0.0275 + 1.061x R = 0.975
MISR Ocean 550 nm
67% within expected error N = 394
0
10
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Salad
11 11
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Motivation?
12 12
• “Overall, about 70% to 75% of MISR AOD retrievals fall within 0.05 or 20% x AOD of the paired validation data from the Aerosol Robotic Network (AERONET), and about 50% to 55% are within 0.03 or 10% x AERONET AOD…” (Kahn et al., 2010)
Nature, 7 November 2013
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Comparison of MISR and MODIS
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Particle/Mixture Issues
14 14
Kahn et al. (2009). MISR aerosol product attributes and statistical comparisons with MODIS, IEEE Transactions on Geoscience and Remote Sensing
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GEOS-‐5 Reanalysis AcOviOes
ICAP 6th Working Group MeeOng, Boulder, CO, October 21 -‐ 24, 2014
Comparison to mulO-‐year satellite data sets
Courtesy of Pete Colarco
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Algorithm Updates (Completed)
19 19
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Algorithm Updates (Completed)
20 20
• Match angular resolution to SMART • Update surface albedo threshold in AOD uppper bound to improve shallow
water coverage • Replace quadratic interpolation with spline in SMART translation • Enhance HET camera selection code to improve coverage in mountains • Revised AOD upper bound mask to account for absorbing particles • Require contiguous grid points in parabolic fit • Calculate chi-square parameters at retrieved AOD (not on grid) • Fix error in variance threshold • Remove log transform in parabolic fit • Lower floor in chi-square uncertainty • Use glitter to retrieve windspeed over dark water (when possible) • Add grid points at low AOD • Eliminate AOD “uncertainty” as successful mixture criterion • Increase Mie code iterations for Particle 6
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Product Updates (Proposed)
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Product Updates (Proposed)
22 22
• Move to 4.4 km x 4.4 km spatial resolution • Separate surface algorithm from aerosol algorithm • Simplify aerosol product
– Separate product into (at least) USER and DIAGNOSTIC file
– Include additional fields (e.g., lat/lon) to make data more user friendly
– Critically examine contents of current product
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MISR PIXLEYCA Local Mode Orbit 69644
Results – San Joaquin Valley, CA 20 Jan 2013
23 23
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AERONET DRAGON Sites 24
N=14
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AERONET DRAGON Sites 25
N=14
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17.6 km Standard Product 26
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4.4 km Local Mode Product 27
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4.4 km Local Mode Product 28
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MISR-‐AERONET nearest Ome to MISR overpass
29
MISR local mode 4.4 km resoluOon
MISR AO
D (558 nm)
AERONET AOD (558 nm)
0 0.05 0.10 0.15 0.20 0.25 0.3
0 0.05 0.10 0.15 0.20 0.25 0.3
N=12 R=0.607845 R2=0.369476 RMSE=0.05461
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MISR-‐AERONET nearest Ome to MISR overpass
MISR local mode 4.4 km resoluOon
MISR AO
D (558 nm)
AERONET AOD (558 nm)
0 0.05 0.10 0.15 0.20 0.25 0.3
0 0.05 0.10 0.15 0.20 0.25 0.3
N=13 R=0.918575 R2=0.843779 RMSE=0.02027
30
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O31948, P143 over India 20 Dec 2005
31
Comparison of 17.6 km and 4.4 km products
V22 17.6 km standard product
Prototype 4.4 km product
AOD
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Comparison of 4.4 km prototype AODs with standard 17.6 km aerosol product
32
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Main
33 33
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0.001 0.010 0.100 1.000
RelaOve Num
ber o
f ParOcles
MODIS Small ParOcles
MISR Small ParOcles ParOcle Radius (µm)
0.001 0.010 0.100 1.000 ParOcle Radius (µm)
RelaOve Num
ber o
f ParOcles
MODIS Large ParOcles
MISR Large ParOcles
RelaOve Num
ber o
f ParOcles
RelaOve Num
ber o
f ParOcles
0.01 0.10 1.000 10.00 ParOcle Radius (µm)
0.01 0.10 1.000 10.00 ParOcle Radius (µm)
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Orbit 37813 Path 084 2007-‐01-‐26
No Successful Matches
Cameras in Glint
Lines Thick = ObservaOons
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Orbit 37813 Path 084
2007-‐01-‐26 246m – Chisq Abs Floor
2.0 m/s Wind NO Geom NO Spec BE AOD: 0.0241 LR AOD: 0.0224
Passing Mixtures: 246 LR Mix: 69
Spherical_Reff_0.12_Med_Dust_Coarse_Dust
χ2abs = 0.1370
Lines Thick = ObservaOons
Thin = Retrieval
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Lines Thick = ObservaOons
Thin = Retrieval
Orbit 37813 Path 084 2007-‐01-‐26
246m – Chisq Abs No Floor 2.0 m/s Wind NO Geom NO Spec
BE AOD: 0.0220 LR AOD: 0.0233
Passing Mixtures: 238 LR Mix: 233
Spherical_Reff_0.12_SSA_green_1.0_Reff_0.06_SSA_green_0.94_Absorbing
χ2abs = 0.2904
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MAN = 0.0244 MISR = 0.1496
MODIS = 0.0240
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MAN = 0.0244 MISR = 0.1496
MODIS = 0.0240
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MAN = 0.0244 MISR = 0.1496
MODIS = 0.0240
MISR Mixture 14 AErg = 1.673 (1.673)
AEmisr = 1.621
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MAN = 0.0244 MISR = 0.1496
MODIS = 0.0240
MODIS ParOcle 1 AErg = 2.726 (2.698)
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MAN = 0.0244 MISR = 0.1496
MODIS = 0.0240
MISR Mixture 14 AErg = 1.673 (1.673)
AEmisr = 1.621
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MAN = 0.0244 MISR = 0.1496
MODIS = 0.0240
MODIS ParOcle 1 AErg = 2.726 (2.698)
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74 Mixtures (Standard Product)
Key Spherical Non-Absorbing
Spherical Absorbing Non-Spherical
Spherical Absorbing + Non-Spherical (Tie)
Spherical Non-Absorbing + Non-Spherical (Tie) Spherical Absorbing + Spherical Non-Absorbing (Tie)
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243 Mixtures (Ralph’s Set)
Key Spherical Non-Absorbing
Spherical Absorbing Non-Spherical
Spherical Absorbing + Non-Spherical (Tie)
Spherical Non-Absorbing + Non-Spherical (Tie) Spherical Absorbing + Spherical Non-Absorbing (Tie)
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243 Mixtures (Ralph’s Set)
Key Spherical Non-Absorbing
Spherical Absorbing Non-Spherical
Smoke+Dust
Medium Mode Non-Absorbing Medium Mode Absorbing
Highly Absorbing
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Standard V22 Het + Homog (246 Mixtures)
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New Het (99%) + New Homog (Tau0 = 1.0)
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Optimization
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Chi-‐Squared Het 2-‐D Plots
Dimensions: x-‐axis = AOD y-‐axis = Mixture Number (74 mixtures)
1 2 Bad Fit 0 Good Fit
AERONET AOD for these cases is shown as a verOcal green line Lowest Chi-‐Squared Het value shown as a symbol (Asterisk) Triplet = (Mixture, AOD, Chi-‐Squared Het) Added Upper Bound Mask and Lowest Chi-‐Squared Value (Triangle)
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Dessert
63 63
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Benford’s Law • Simon Newcomb (pictured) published an arOcle in the American Journal of
MathemaOcs in 1881 aeer noOcing that books of logarithms in the library were more used at the beginning and progressively lesser used. He inferred that scienOsts were looking up numbers starOng with 1 more oeen and less oeen for later numbers. He expressed this mathemaOcally with the equaOon:
• Frank Benford (not pictured) rediscovered this law by making exactly the same observaOon about books of logarithms and found many other data sets that followed the law. He published his results in a paper in the Proceedings of the American Philosophical Society in 1938.
!
PD = log10 1+1 D( )
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Benford’s Law
Sambridge et al., GRL, 2010
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Matched MISR V22/AERONET Data
Line shows predictions from Benford’s Law
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Matched MISR V22/
MODIS Data
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References
68 68
Diner, D. J., et al. (2005), Using angular and spectral shape similarity constraints to improve MISR aerosol and surface retrievals over land, Remote Sens. Environ., 94, 155-171.
Kahn, R. A., et al. (2009), MISR aerosol product attributes and statistical comparisons with MODIS, IEEE Trans. Geosci. Remote Sens., 47, 4095-4114.
Kahn, R. A., et al. (2010), Multiangle Imaging SpectroRadiometer global aerosol product assessment by comparison with the Aerosol Robotic Network, J. Geophys. Res., 115, D23209, doi:10.1029/2010JD014601.
Diner, D. J., et al. (2012), An optimization approach for aerosol retrievals using simulated MISR radiances, Atmos. Res., 116, 1-14.
Kalashnikova, O. V., et al. (2013), MISR Dark Water aerosol retrievals: operational algorithm sensitivity to particle non-sphericity, Atmos. Meas. Tech., 6, 2131-2154.
Sambridge, M., et al. (2010), Benford’s law in the natural sciences,
Geophys. Res. Lett., 37, L22301, doi:10.1029/2010GL044830.