Magnetospheric Convection as Observed by the Electron Drift Instrument (EDI) on Cluster Compared With Ground-based Radar Data

Details Magnetospheric Convection as Observed by the Electron Drift Instrument (EDI) on Cluster Compared With Ground-based Radar Data Magnetospheric Convection as Observed by the Electron Drift Instrument (EDI) on Cluster Compared With Ground-based Radar Data

Dec 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001agufmsm22a0814f&link_type=abstract

American Geophysical Union, Fall Meeting 2001, abstract #SM22A-0814

Physics

2712 Electric Fields (2411), 2740 Magnetospheric Configuration And Dynamics, 2794 Instruments And Techniques

Scientific paper

Storms and substorms in the magnetosphere are accompanied by enhanced magnetospheric electric fields associated with an increase in convection and intensified wave activity. New data from the Electron Drift Instruments (EDI) of the Cluster mission will be presented. They comprise several outbound Cluster orbits above the Northern polar cap up to the magnetopause. These measurements will be related to corresponding ground-based data from the Superdarn radars and the Sondrestrom incoherent scatter radar.

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