Ionospheric peak height at the magnetic equator: Comparison between ionosonde measurements and IRI

© 2016 COSPAR The ionospheric peak height in the F layer (hmF2) varies with not only thermospheric conditions but also dynamic processes in the upper atmosphere. At mid-latitudes, the field-aligned diffusion and recombination loss determine the hmF2 in the absence of applied vertical drift. Vertical...

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Bibliographic Details
Main Authors: Maruyama T., Ma G., Tsugawa T., Supnithi P., Komolmis T.
Format: Journal
Published: 2017
Online Access:https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85020899499&origin=inward
http://cmuir.cmu.ac.th/jspui/handle/6653943832/40275
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Institution: Chiang Mai University