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Freja observations of heating and precipitation of positive ions
Author(s) -
Eliasson L.,
André M.,
Eriksson A.,
Norqvist P.,
Norberg O.,
Lundin R.,
Holback B.,
Koskinen H.,
Borg H.,
Boehm M.
Publication year - 1994
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/94gl01067
Subject(s) - ion , ionosphere , hiss , field line , physics , electron precipitation , pitch angle , plasma , proton , atomic physics , computational physics , transverse plane , anisotropy , geophysics , electron , atmospheric sciences , magnetosphere , nuclear physics , optics , structural engineering , quantum mechanics , engineering
The experiments on board Freja are designed to measure auroral particle energization processes with very high temporal and spatial resolution. One main scientific objective is to study ion heating transverse to the magnetic field lines in the auroral region. The Freja orbit with an inclination of 63° allows us to make detailed measurements in the nightside auroral oval during all disturbance levels. We concentrate here on two different observations of transverse ion energization at an altitude of about 1700 km in the northern hemisphere auroral region. The three‐dimensional ion mass spectrograph has shown that both heavy and light ions are heated to energies most often in the range from a few eV to some hundred eV. Transversely heated ions are, however, also seen up to the present high energy limit of the hot plasma instrument, 4.5 keV. Ion conics are produced in regions with anisotropic electron fluxes as well as in regions of intense keV proton precipitation. Waves above the lower hybrid frequency are observed in the events presented in this report. These waves may play an important role in the ion heating process. The Freja data indicate that the waves are generated in different ways in these events. Thus, this preliminary investigation confirms that several scenarios are needed to explain the heating of ionospheric plasma and shows some of the possibilities for future studies.