Wednesday, 25 January 2017: 1:45 PM
Conference Center: Skagit 4 (Washington State Convention Center )
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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