10.2 Using CATS Near-Realtime Lidar Observations to Monitor and Constrain Volcanic Sulfur Dioxide (SO2) Forecasts

Wednesday, 25 January 2017: 1:45 PM
Conference Center: Skagit 4 (Washington State Convention Center )
Eric Hughes, University of Maryland, College Park, MD; and J. E. Yorks, N. A. Krotkov, A. Da Silva, and M. J. McGill

An eruption of the Italian volcano Mt. Etna on December 3rd, 2015 produced a large sulfur dioxide (SO2) and sulfate aerosol cloud that travelled across Asia, eventually reaching North America.  The Ozone Profiler and Mapping Suite (OMPS) aboard the National Polar-orbiting Partnership (Suomi-NPP) satellite observed the horizontal transport of the SO2 cloud. Vertical profiles of the co-located sulfate aerosols were observed between 11.5km - 14km by the new Cloud Aerosol Transport System (CATS) space-based LIDAR aboard the International Space Station (ISS).  Backward trajectory analysis estimates the altitude of the SO2 cloud much lower, at 7 – 12km.  Eulerian model simulations of the SO2 cloud constrained by CATS measurements produced more accurate dispersion patterns compared to those initialized with the back trajectory only height estimate.  The near-realtime data processing capabilities of CATS is unique, and this work provides a first time usage of these observations to monitor and model volcanic clouds.
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