Location of Pc 1–2 waves relative to the magnetopause
Spacecraft-borne and ground-based magnetometers frequently detect magnetospheric micropulsations in the period range 0.2–10 s, termed Pc 1–2, and attributed to electromagnetic ion cyclotron waves driven by temperature anisotropy (<i>T</i><font face="Symbol" ><su...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2002-11-01
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Series: | Annales Geophysicae |
Online Access: | https://www.ann-geophys.net/20/1763/2002/angeo-20-1763-2002.pdf |
Summary: | Spacecraft-borne and
ground-based magnetometers frequently detect magnetospheric micropulsations in
the period range 0.2–10 s, termed Pc 1–2, and attributed to electromagnetic
ion cyclotron waves driven by temperature anisotropy (<i>T</i><font face="Symbol" ><sub>^</sub></font>
> T <font face="Symbol" ><sub>||</sub></font>). Previous surveys of
Pc 1 occurrence locations have been limited to L <u><</u> 9. We
present AMPTE/IRM observations of the distribution of Pc 1 waves out to the
magnetopause, for a limited region of MLT = 10–14. The probability of wave
occurrence <i>P</i><sub>wav</sub> is large (> 0.15) between <i>L</i> = 7–12,
peaking at <i>L</i> = 8–10 (<i>P</i><sub>wav</sub> ~ 0.25). When the <i>L</i>-value
is normalized to the magnetopause position <i>L</i><sub>mp</sub>, however, the
highest probabilities of Pc 1 wave occurrence are close to the magnetopause,
with <i>P</i><sub>wav</sub> ~0.25 for <i>L</i><sub>norm</sub> <u>=</u> <i>L/L</i><sub>mp</sub>
= 0.8–1.0. These results are consistent with increased convective growth rate
at large <i>L</i> and with the greater effect of magnetosphere compression
close to the magnetopause. On the other hand, we only directly observe magnetic
field compression for at most about 25% of the wave events.<br><br><b>Key words. </b>Magnetospheric physics (magnetospheric
configuration and dynamics; MHD waves and instabilities; plasma waves and
instabilities) |
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ISSN: | 0992-7689 1432-0576 |