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The space shuttle main engine plume deposited between 100 and 115\ km altitude is a valuable tracer for global-scale dynamical processes. Several studies have shown that this plume can reach the Arctic or Antarctic to form bursts of polar mesospheric clouds (PMCs) within a few days. The rapid transport of the shuttle plume is currently not reproduced by general circulation models and is not well understood. To help delineate the issues, we present the complete satellite datasets of shuttle plume observations by the S ...
Published by: Journal of Atmospheric and Solar-Terrestrial Physics Published on: 02/2014
YEAR: 2014   DOI: 10.1016/j.jastp.2013.12.004