Aerosol plume after the Chelyabinsk bolide |
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Authors: | N N Gorkavyi T A Taidakova E A Provornikova I N Gorkavyi M M Akhmetvaleev |
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Institution: | 1. Science Systems and Applications, Inc., Lanham, USA 2. Greenwich Institute for Science and Technology, Haymarket, USA 3. Institute of Space Research, Russian Academy of Sciences, Moscow, Russia 4. Boston University, Boston, USA
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Abstract: | In this work, the bolide is studied as an atmospheric event causing significant release of meteoritic dust into the stratosphere. Ground-based pictures taken by eyewitnesses and images from the Japan geostationary satellite MTSAT-2 are used as a database. The analysis of the ground-based pictures allows the altitude of the main burst to be estimated as 22.9 ± 1.6 km. It is shown that the top of the cloud formed due to the main burst rose to 11 km for about 60–80 s due to convection, which provides an estimate of the maximum vertical velocity of 130–180 m/s. According to calculations, the upper part of the trail is affected by a strong wind drift and is located at an altitude of >53 km, in the mesosphere. The MTSAT-2 data show that the mesospheric part of the trail traveled southwestward, while the stratospheric part, northeastward, with velocities higher than 100 km/h. |
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