H.: Simulation of the October-November 2003 solar proton events in the CMAM GCM: Comparison with observations, Geophys. Res

NOx in the lower polar mesosphere, in mid February of 2004, more than 100 times normal. Using a middle atmosphere GCM we investigate whether solar proton events or subsequent associated aurorae can explain the NOx observations. We find that the solar proton events produce insufficient amounts of NOx...

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Bibliographic Details
Main Authors: K. Semeniuk, J. C. Mcconnell, C. H. Jackman
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.664.2798
http://www.ace.uwaterloo.ca/publications/2005/SemeniukSPEreprint.pdf
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Summary:NOx in the lower polar mesosphere, in mid February of 2004, more than 100 times normal. Using a middle atmosphere GCM we investigate whether solar proton events or subsequent associated aurorae can explain the NOx observations. We find that the solar proton events produce insufficient amounts of NOx, less than 2 ppmv at 90 km. However, it is likely that intense aurorae associated with the Oct.–Nov. 2003 solar storms, and their aftermath, produced thermospheric values of NOx reaching hundreds of ppmv. In addition, from our simulations we infer that NOx rich air must have experienced unusually confined polar night descent in the mesosphere in December and