Non-thermal plasma observations using EISCAT: Aspect angle dependence


Autoria(s): Winser, K. J.; Lockwood, Mike; Jones, G. O. L.
Data(s)

1987

Resumo

Recent observations with the EISCAT incoherent scatter radar have shown large rises in dayside, auroral plasma velocities (>2 km s^{−1}) over a wide range of latitudes and lasting about an hour. These are larger than the neutral thermal speed, and allow, for the first time, observations of a non-thermal plasma over a range of observing angles, revealing a clear angular dependence. The observed ion temperature anisotropy, deduced by assuming a Maxwellian line-of-sight ion velocity distribution, is at least 1.75, which exceeds the theoretical value for a bi-Maxwellian based on a realistic ion-neutral collision model. The aspect angle dependence of the signal spectra also indicates non-Maxwellian plasma.

Formato

text

Identificador

http://centaur.reading.ac.uk/38898/1/34_Winseretal_1987.pdf

Winser, K. J., Lockwood, M. <http://centaur.reading.ac.uk/view/creators/90001127.html> and Jones, G. O. L. (1987) Non-thermal plasma observations using EISCAT: Aspect angle dependence. Geophysical Research Letters, 14 (9). pp. 957-960. ISSN 0094-8276 doi: 10.1029/GL014i009p00957 <http://dx.doi.org/10.1029/GL014i009p00957>

Idioma(s)

en

Publicador

American Geophysical Union

Relação

http://centaur.reading.ac.uk/38898/

creatorInternal Lockwood, Mike

http://dx.doi.org/10.1029/GL014i009p00957

10.1029/GL014i009p00957

Tipo

Article

PeerReviewed