Abstract
The STARE radar system has for the first time been used to study Pi 2 pulsations associated with substorm onsets. Such pulsations have a period which typically makes them only marginally observable with STARE; nevertheless, an event has been identified. The spatial and temporal variations of the observed ionospheric flow vectors, and consequently also the electric field vectors, are complex and require further study, but are qualitatively comparable to model predictions. Magnetic field oscillations computed from the STARE data using the Biot-Savart law correlate well with magnetometer data.
Sign-in/Register to access full text options 
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.
