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A Fast and Sensitive New Satellite SO2 Retrieval Algorithm based on Principal Component Analysis: Application to the Ozone Monitoring InstrumentWe describe a new algorithm to retrieve SO2 from satellite-measured hyperspectral radiances. We employ the principal component analysis technique in regions with no significant SO2 to capture radiance variability caused by both physical processes (e.g., Rayleigh and Raman scattering and ozone absorption) and measurement artifacts. We use the resulting principal components and SO2 Jacobians calculated with a radiative transfer model to directly estimate SO2 vertical column density in one step. Application to the Ozone Monitoring Instrument (OMI) radiance spectra in 310.5-340 nm demonstrates that this approach can greatly reduce biases in the operational OMI product and decrease the noise by a factor of 2, providing greater sensitivity to anthropogenic emissions. The new algorithm is fast, eliminates the need for instrument-specific radiance correction schemes, and can be easily adapted to other sensors. These attributes make it a promising technique for producing longterm, consistent SO2 records for air quality and climate research.
Document ID
20140011341
Acquisition Source
Goddard Space Flight Center
Document Type
Reprint (Version printed in journal)
External Source(s)
Authors
Li, Can
(Maryland Univ. College Park, MD, United States)
Joiner, Joanna
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Krotkov, A.
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Bhartia, Pawan K.
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Date Acquired
September 3, 2014
Publication Date
November 22, 2013
Publication Information
Publication: Geophysical Research Letters
Volume: 40
Issue: 23
Subject Category
Geosciences (General)
Report/Patent Number
GSFC-E-DAA-TN11412
Funding Number(s)
CONTRACT_GRANT: NNX12AD03A
Distribution Limits
Public
Copyright
Public Use Permitted.
Keywords
Principal component analysis
Sulfur dioxide
Ozone Monitoring Instrument (OMI)
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