“…These waves, which are continually radiated outward from the BBFs to the auroral oval, are found to be a very efficient plasma sheet energy loss process [ Chaston et al , ; Ergun et al , ], transferring the energy from the fields to the plasma [ Huang et al , ; Angelopoulos et al , ]. Whistlers have been previously recorded on board Cluster [ Khotyaintsev et al , ; Huang et al , ] and Time History of Events and Macroscale Interactions during Substorms (THEMIS) [ Le Contel et al , ; Deng et al , ] and are thought to be generated by the perpendicular electron temperature anisotropy resulting from betatron acceleration that occurs as the magnetic field strength increases inside the FPR [see, e.g., Wu et al , ; Fu et al , ; Huang et al , ; Wu et al , ]. Deng et al [] investigated the properties (namely, propagation angle, degree of polarization, and ellipticity) of whistler waves inside the magnetotail FPR, and by analyzing Poynting flux, Khotyaintsev et al [] have shown that these waves are generated near the geomagnetic equator.…”