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Poststorm Thermospheric NO Overcooling?
Author(s) -
Mikhailov Andrey V.,
Perrone Loredana
Publication year - 2020
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1029/2019ja027122
Subject(s) - storm , atmospheric sciences , atomic oxygen , ionosphere , environmental science , meteorology , oxygen , physics , geophysics , quantum mechanics
A mechanism of the neutral gas density decrease at middle latitudes during the recovery storm phase is discussed. The recently proposed method to retrieve thermospheric parameters from ionospheric observations is used for the analysis of equinoctial, summer, and winter severe magnetic storms. CHAllenging Minisatellite Payload and Swarm neutral gas density observations are used for a comparison. It is shown that storm‐induced atomic oxygen variation is the controlling process. Well‐known F 2 ‐layer storm morphology and the poststorm decrease of neutral gas density reflect the same storm‐induced variations of atomic oxygen abundance in the upper atmosphere. There is no need to attract a new “poststorm NO overcooling” concept to explain the decrease of neutral gas density.