Abstract This study employs the Horizontal Wind model 2014 to calculate the intensity of the Vertical ion convergence (VIC) to examine the role of neutral wind shear in the global distribution of the Es occurrence rate. The global S4 observations from the FORMOSAT-3/COSMIC GPS Occultation Experiment (GOX) are used to derive global information on the Es occurrence. Both the simulation and observation suggest that the Es highly occurs in the mid-latitude regions of the summer hemisphere.
Comparison of global morphologies of vertical ion convergence and sporadic E occurrence rate
Advances in Space Research ; 63 , 11 ; 3606-3611
2019-02-18
6 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
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