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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 100, NO. A12,
PAGES 23,397–23,412,
1995
Regions of Abnormally Low Proton Temperature in the Solar Wind (1965-1991) and their Association with Ejecta
I. G. Richardson
Also at Department of Astronomy, University of Maryland, College Park.
H. V. Cane
Also at Physics Department, University of Tasmania, Hobart, Tasmania, Australia.
Abstract
Occurrences of solar wind plasma with abnormally low proton temperatures (Tp ) have long been associated with the interplanetary manifestations (which we term “ejecta”) of coronal mass ejections (CMEs).
We survey the National Space Science Data Center Omni solar wind database for 1965-1991, and data from the Helios 1 and 2
spacecraft for more limited periods, to identify plasma in which Tp is less than the temperature expected (Tex ) from the well-established correlation between the solar wind speed and Tp for normal solar wind expansion. The occurrence rate of low-temperature plasma (specifically with Tp /Tex ≤ 0.5) is shown to be correlated with solar activity levels. Individual low-temperature regions have durations from 1 to
∼80 hours with a mean of ∼10 hours. Around one third are encounters with the heliospheric plasma sheet (HPS). These events
are observed most frequently during the increasing phase of solar activity when the HPS lies closer to the ecliptic. The abnormally
low temperatures may be intrinsic to the HPS or may provide support for the proposal that the coronal streamer belt underlying
the HPS is a frequent source of ejecta. The remaining events have an occurrence rate which shows a particularly clear correlation
with solar activity levels and with the CME rate at the Sun (when CME observations are available), consistent with an association
with ejecta. These events also show greater than chance associations with other ejecta signatures. We suggest that the Omni
plasma data can provide information on the rate of ejecta passing the Earth, and hence give an indication of the CME rate,
for a period commencing before spacecraft coronagraph CME observations became available in the early 1970s. Our findings suggest
that Tp depressions may provide a more comprehensive indication of the presence of ejecta than other ejecta signatures, such as bidirectional
solar wind electron heat fluxes and energetic ion flows, which alone do not identify all ejecta.
Received 27
October
1994;
accepted 29
August
1995.
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Citation: Richardson, I. G., and H. V. Cane
(1995),
Regions of Abnormally Low Proton Temperature in the Solar Wind (1965-1991) and their Association with Ejecta,
J. Geophys. Res.,
100(A12),
23,397–23,412.
Copyright 1995 by the American Geophysical Union.
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