What Local Sub-auroral Ionospheric Electron Temperature Enhancements Tell Us about MI Coupling C. Gurgiolo, B. Sandel, X.X. Zhang, J. Perez, P. Brandt, and J-M. Jahn Local enhancements in the sub-auroral ambient ionospheric electron temperature are common during disturbed times. Current thinking has it that these result from a downward directed heat flux generated either by instabilities active in the region where the ring current overlaps the plasmasphere or by Coulomb scattering of the plasmaspheric electrons off the heavier ring current ions. In this talk we look at sub-auroral ionospheric heating events in the context of the plasmasphere and ring current to see what they can tell us about MI coupling. Data from the IMAGE satellite provides global plasmasphere and ring current maps and data from the DMSP satellite provides in-situ ionospheric conditions in the study. We find that heating events separate into three categories which we call inner, conjugate outer and non-conjugate outer events. Inner events occur well inside the plasmasphere boundary layer and are mostly observed in the dawn/noon sectors; conjugate outer events occur within the plasmasphere boundary layer, primarily in the dusk/midnight sectors and mainly in the substorm growth and early recovery phases; and non-conjugate outer events are broad regions of heating, often extending beyond the plasmapause and are observed primarily in the dusk/midnight sectors late in the recovery phase. The mechanism providing the heat flux in each category does not appear to be the same, in fact, only with conjugate outer events does it appear that the conventional models play a role. With inner events the equatorial hot to cold density ratio is to small to sustain EMIC waves. With non-conjugate outer events the non-conjugacy argues against an equatorial source and the extension beyond the plasmapause decouples the plasmasphere from the ring-current. One possibility which will be explored in the case of non-conjugate outer events is that the heating is related to processes active in the refilling of the plasmaspheric flux-tubes. _______________ Global Aspects of Magnetosphere-Ionosphere Coupling, 2006 Yosemite Workshop, Yosemite National Park, CA, USA, 7-10 February 2006