HR: 0800h
AN: V31A-0293    [Abstracts]
TI: The NOAA Near Real-time OMI-SO2 Cloud Visualization and Product Distribution System
AU: * Vicente, G
EM: Gilberto.Vicente@noaa.gov
AF: NOAA/NESDIS - Office of Satellite Data Processing and Distribution - OSDPD, Suite 510, E/SP22 5200 Auth Road, Camp Springs, 20746, United States
AU: Serafino, G
AF: NOAA/NESDIS - Office of Satellite Data Processing and Distribution - OSDPD, Suite 510, E/SP22 5200 Auth Road, Camp Springs, 20746, United States
AU: Krueger, A
AF: Joint Center for Earth Systems Technology, University of Maryland Baltimore County, JCET - UMBC, 1000 Hilltop Circle, Baltimore, MD 21250, United States
AU: Carn, S
AF: Joint Center for Earth Systems Technology, University of Maryland Baltimore County, JCET - UMBC, 1000 Hilltop Circle, Baltimore, MD 21250, United States
AU: Yang, K
AF: Joint Center for Earth Systems Technology, University of Maryland Baltimore County, JCET - UMBC, 1000 Hilltop Circle, Baltimore, MD 21250, United States
AU: Krotkov, N
AF: Goddard Earth Science and Technology Center, GEST - UMBC, 5523 Research Park Drive, Suite 320, Baltimore, MD 21228, United States
AU: Guffanti, M
AF: U.S. Geological Survey (USGS), 926A National Center, Reston, VA 20192, United States
AU: Levelt, P
AF: Royal Netherlands Meteorological Institute - KNMI, Wilhelminalaan 10, De Bilt, GK NL-3732, Netherlands
AB: The Ozone Monitoring Instrument (OMI) on the NASA EOS/Aura research satellite allows measurement of SO2 concentrations at UV wavelengths with daily global coverage. SO2 is detected from space using its strong absorption band structure in the near UV (300-320 nm) as well as in IR bands near 7.3 and 8.6 mm. Thirty years of UV SO2 measurements with the Total Ozone Mapping Spectrometer (TOMS) and OMI sensors have shown that the highest concentrations of SO2 occur in volcanic clouds produced by explosive magmatic eruptions, which also emit ash. However, icing of ash particles in water-rich eruption clouds, and/or suppression of the IR split- window signal by ambient water vapor or cloud opacity can inhibit direct detection of ash from space. Large SO2 concentrations are therefore a reliable indicator of the presence of airborne volcanic ash. UV SO2 measurements are very robust and are insensitive to the factors that confound IR data. SO2 and ash can be detected in a very fresh eruption cloud due to sunlight backscattering and ash presence can be confirmed by UV derived aerosol index measurements. The lack of other large point sources of SO2 facilitates development and implementation of automated searches for volcanic clouds with a very low false alarm rate. The NASA Earth Sciences Applications Office has funded a cooperative agreement between UMBC, NOAA, GSFC, and USGS to infuse research satellite SO2 data products into volcanic hazard Decision Support Systems (DSSs) operated by the National Oceanic and Atmospheric Administration (NOAA) and the US Geological Survey (USGS). This will provide aviation alerts to the Federal Aviation Administration (FAA), that will reduce false alarms and permit more robust detection and tracking of volcanic clouds, and includes the development of an eruption alarm system, and potential recognition of pre-eruptive volcanic degassing. Near real-time (NRT) observations of SO2 and volcanic ash can therefore be incorporated into data products compatible with Decision Support Tools (DSTs) in use at Volcanic Ash Advisory Centers (VAACs) in Washington and Anchorage, and the USGS Volcano Observatories. In this poster we show the latest NOAA Office of Satellite Data Processing and Distribution (OSDPD) development of an online NRT image and data product distribution system that generates eruption alarms, allows the extraction of volcanic cloud subsets for special processing, and provides access to analysis tools and graphical products. Products are infused into DSTs including the Volcanic Ash Coordination Tool (VACT), under development by the NOAA Forecast Systems Laboratory and the FAAs Oceanic Weather Product Development Team (OWPDT), to monitor and track, drifting volcanic clouds.
DE: 0305 Aerosols and particles (0345, 4801, 4906)
DE: 8409 Atmospheric effects (0370)
DE: 8419 Volcano monitoring (7280)
DE: 8485 Remote sensing of volcanoes
DE: 8488 Volcanic hazards and risks
SC: Volcanology, Geochemistry, Petrology [V]
MN: 2007 Fall Meeting