Dissertations and Theses 9-2014 Ion-Cyclotron Resonance Heating of O+ in the Topside Ionosphere and Mapping Outflows ot the Magnetosphere Anthony W. Pritchard Follow this and additional works at: https://commons.erau.edu/edt Part of the Atmospheric Sciences Commons, and the Engineering Physics Commons Scholarly Commons Citation Pritchard, Anthony W., "Ion-Cyclotron Resonance Heating of O+ in the Topside Ionosphere and Mapping Outflows ot the Magnetosphere" (2014). Dissertations and Theses. 234. https://commons.erau.edu/edt/234 This Thesis - Open Access is brought to you for free and open access by Scholarly Commons. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of Scholarly Commons. For more information, please contact
[email protected]. ION-CYCLOTRON RESONANCE HEATING OF O+ IN THE TOPSIDE IONOSPHERE AND MAPPING OUTFLOWS TO THE MAGNETOSPHERE BY ANTHONY W. PRITCHARD A Thesis Submitted to the Department of Physical Sciences and the Committee on Graduate Studies In partial fulfillment of the requirements for the degree of Master in Science in Engineering Physics 09/2014 Embry-Riddle Aeronautical University Daytona Beach, Florida c Copyright by Anthony W. Pritchard 2014 All Rights Reserved ii Abstract This thesis considers the heavy ion dynamics due to ion-cyclotron resonance en- ergization processes that take place in the turbulent region of the Earth’s topside, high latitude ionosphere. We simulate the impact of this transverse heating process upon energies and velocity distribution functions of outflowing oxygen ions (O+) in the approximate altitude range of 800 km to 15,000 km. To do so most effectively, we use a single particle tracing model that precisely reproduces the small-scale wave-particle interaction of broadband extremely low frequency (BBELF) waves with the ions’ cyclotron motions, leading to the upward acceleration of ions in type-II ion outflows and ion conics.