Abstract
Storm-time variations of electron content measured at Auckland, New Zealand and of F2-layer critical frequency measured at Australasian stations have been examined. Increases of electron content are found to be associated with a class of ‘S-events’ which are defined in terms of magnetic D st variations. The results of previously published storm-time variations have been reconsidered. It is suggested that the variety of forms of F2-layer storm variations is due to the coexistence of two opposing effects on electron concentrations.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
