A new discrete wavelength backscattered ultraviolet algorithm for consistent volcanic SO<sub>2</sub> retrievals from multiple satellite missions
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Published:2019-09-25
Issue:9
Volume:12
Page:5137-5153
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ISSN:1867-8548
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Container-title:Atmospheric Measurement Techniques
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language:en
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Short-container-title:Atmos. Meas. Tech.
Author:
Fisher Bradford L.ORCID, Krotkov Nickolay A.ORCID, Bhartia Pawan K., Li Can, Carn Simon A.ORCID, Hughes Eric, Leonard Peter J. T.
Abstract
Abstract. This paper describes a new discrete wavelength algorithm
developed for retrieving volcanic sulfur dioxide (SO2) vertical column
density (VCD) from UV observing satellites. The Multi-Satellite SO2
algorithm (MS_SO2) simultaneously retrieves column densities
of sulfur dioxide, ozone, and Lambertian effective reflectivity (LER) and its
spectral dependence. It is used operationally to process measurements from
the heritage Total Ozone Mapping Spectrometer (TOMS) onboard NASA's
Nimbus-7 satellite (N7/TOMS: 1978–1993) and from the current Earth
Polychromatic Imaging Camera (EPIC) onboard Deep Space Climate Observatory
(DSCOVR: 2015–ongoing) from the Earth–Sun Lagrange (L1) orbit. Results from
MS_SO2 algorithm for several volcanic cases were assessed
using the more sensitive principal component analysis (PCA) algorithm. The
PCA is an operational algorithm used by NASA to retrieve SO2 from
hyperspectral UV spectrometers, such as the Ozone Monitoring Instrument (OMI) onboard NASA's Earth Observing System Aura satellite and Ozone Mapping and
Profiling Suite (OMPS) onboard NASA–NOAA Suomi National Polar Partnership
(SNPP) satellite. For this comparative study, the PCA algorithm was
modified to use the discrete wavelengths of the Nimbus-7/TOMS instrument,
described in Sect. S1 of the Supplement. Our results demonstrate good
agreement between the two retrievals for the largest volcanic eruptions of
the satellite era, such as the 1991 Pinatubo eruption. To estimate SO2
retrieval systematic uncertainties, we use radiative transfer simulations
explicitly accounting for volcanic sulfate and ash aerosols. Our results
suggest that the discrete-wavelength MS_SO2 algorithm,
although less sensitive than hyperspectral PCA algorithm, can be adapted to
retrieve volcanic SO2 VCDs from contemporary hyperspectral UV
instruments, such as OMI and OMPS, to create consistent, multi-satellite,
long-term volcanic SO2 climate data records.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference58 articles.
1. Ahmad, Z. and Bhartia, P. K.: Effect of Molecular anisotropy on the
backscattered UV radiance, Appl. Optics, 34, 8309–8314,
https://doi.org/10.1364/AO.34.008309, 1995. 2. Ahmad, Z., Bhartia P. K., and Krotkov, N. A.: Spectral properties of
backscattered UV radiation in cloudy atmospheres, J. Geophys. Res.-Atmos., 109, D01201,
https://doi.org/10.1029/2003JD003395, 2004. 3. Bhartia, P. K. (Ed.): OMI Algorithm Theoretical Basis Document, Vol. II,
Ozone Products, available at: https://disc.gsfc.nasa.gov/datasets/OMTO3_V003/summary?keywords=OMTO3 (last access: 11 September 2019), 2002. 4. Bobrowski, N., Honninger, G., Galle, B., and Platt, U.: Detection of bromine
monoxide in a volcanic plume, Nature, 423, 273–276, http://https://doi.org/10.1038/nature01625, 2003. 5. Bogumil, K., Orphal, J., Homann, T., Voigt, S., Spietz, P., Fleischmann,
O. C., Vogel, A., Hartmann, M. Kromminga, H., Bovensmann, H., Frerick, J.,
Burrows J. P.: Measurements of molecular absorption spectra with the
SCIAMACHY pre-flight model: instrument characterization and reference data
for atmospheric remote-sensing in the 230–2380 nm region, J. Photoch. Photobio. A, 157, 167–184,
https://doi.org/10.1016/S1010-6030(03)00062-5, 2003.
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