The subauroral heat input to the topside ionosphere from two superthermal e
lectron sources, photoelectrons and plasma sheet electrons, are calculated
using a global kinetic model of electron transport in the inner magnetosphe
re. Peak rates above 10(10) eV cm(-2) s(-1) are found for photoelectrons in
the midlatitude afternoon region, while the peak deposition rate for plasm
a sheet electrons only occasionally approaches 10(9) eV cm(-2) s(-1), and i
s typically confined to the morningside. Trapped clouds of plasma sheet ele
ctrons, however, are shown to have lasting effects on the structure of tops
ide heat input, as the energetic electrons corotate and slowly transfer the
ir energy to the thermal plasma over a course of days. These energy inputs
are compared with other heat sources in the inner magnetosphere. It is conc
luded that, while other processes can inject large amounts of energy into t
he ionosphere in spatially and temporally localized regions, photoelectrons
are the strongest and steadiest heat source into the topside ionosphere. (
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