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Ulysses electron distributions fitted with Kappa functions
DOI: 10.1029/97GL00992 Bibcode: 1997GeoRL..24.1151M

Maksimovic, Milan; Riley, Pete; Pierrard, Viviane

We fit Kappa functions to 16,000 velocity distribution functions measured in the solar wind by the electron plasma instrument on board Ulysses. Statistically, the electron distributions are observed to have important high velocity tails in the fast solar wind but are closer to a Maxwellian in the slow wind. We also discuss how this result could su…

1997 Geophysical Research Letters
Ulysses 375
SWICS/Ulysses observations: The three-dimensional structure of the heliosphere in the declining/minimum phase of the solar cycle
DOI: 10.1029/97GL01605 Bibcode: 1997GeoRL..24.2885W

Livi, S.; Woch, J.; Geiss, J. +5 more

The ESA/NASA spacecraft Ulysses provides the first in-situ observation of the solar wind at high solar latitudes. Data obtained with the Solar Wind Ion Composition Spectrometer (SWICS) during the first orbit of Ulysses around the Sun can be used to obtain a global view of the solar wind pattern within the heliosphere during the declining/minimum p…

1997 Geophysical Research Letters
Ulysses 59
Extension of coronal structure into interplanetary space
DOI: 10.1029/97GL01156 Bibcode: 1997GeoRL..24.1159W

Habbal, Shadia Rifai; Woo, Richard

We investigate the extension and evolution of the solar corona into interplanetary space by comparing 1995 Ulysses radio occultation measurements of path-integrated electron density and density fluctuations measured between 21 and 32 Ro, with simultaneous white-light measurements made by the HAO Mauna Loa K-coronameter below 2.5 Ro…

1997 Geophysical Research Letters
Ulysses 49
The northern edge of the band of solar wind variability: Ulysses at ∼4.5 AU
DOI: 10.1029/97GL00001 Bibcode: 1997GeoRL..24..309G

McComas, D. J.; Goldstein, B. E.; Bame, S. J. +4 more

Ulysses observations reveal that the northern edge of the low-latitude band of solar wind variability at ∼4.5 AU was located at N30° in the latter part of 1996 when solar activity was at a minimum. This edge latitude is intermediate between edge latitudes found during previous encounters with the band edge along different portions of Ulysses' pola…

1997 Geophysical Research Letters
Ulysses 43
Ulysses observations of the northward extension of the heliospheric current sheet
DOI: 10.1029/97GL03099 Bibcode: 1997GeoRL..24.3101F

Balogh, A.; Forsyth, R. J.; Smith, E. J. +1 more

After passing through the northern polar regions of the heliosphere during the summer of 1995, the Ulysses spacecraft has been gradually returning towards lower equatorial latitudes, reaching 30°N in August 1996 at about which time low speed solar wind from the streamer belt was once again observed. This paper reports on the Ulysses magnetic field…

1997 Geophysical Research Letters
Ulysses 30
Particle acceleration at corotating reverse shocks in the southern hemisphere: Ulysses results
DOI: 10.1029/97GL00862 Bibcode: 1997GeoRL..24.1155D

Balogh, A.; Forsyth, R. J.; Desai, M. I. +3 more

We have correlated the ∼1 MeV proton intensity (J) measured at corotating reverse shocks detected by Ulysses in the southern hemisphere with two parameters that characterise the strength of the shock. Between 6°-29°S J is essentially independent of the shock strength, whereas between 29°-41°S J is well correlated with the same. The poor correlatio…

1997 Geophysical Research Letters
Ulysses 13
Ulysses observations of a discrete wavepacket upstream of an interplanetary shock
DOI: 10.1029/97GL52471 Bibcode: 1997GeoRL..24.2387L

Balogh, A.; Lucek, E. A.

We present a single example of a previously unidentified type of upstream wave structure, found several minutes ahead of a forward propagating, oblique interplanetary shock observed on day 6, 1992, using Ulysses magnetometer data. The wave appears as an isolated high frequency wavepacket associated with a larger scale compressive structure. In the…

1997 Geophysical Research Letters
Ulysses 12
The Ulysses north polar pass: Latitudinal gradients of anomalous cosmic ray O, N And Ne
DOI: 10.1029/97GL01747 Bibcode: 1997GeoRL..24.1719T

Sanderson, T. R.; Marsden, R. G.; Trattner, K. J.

A key finding of the Ulysses mission has been the absence of large latitudinal gradients in the Anomalous Cosmic Ray (ACR) component. Studies using data from several satellites have consistently shown a small (∼ 2%/deg.) positive latitudinal gradient for anomalous O, N and Ne in the energy range 4 to 30 MeV/n, and even smaller gradients for ACR He…

1997 Geophysical Research Letters
Ulysses 6
Ulysses observations of short-period (≤30 Days) modulation of the galactic cosmic rays
DOI: 10.1029/97GL00129 Bibcode: 1997GeoRL..24..671B

Keppler, E.; Kunow, H.; Heber, B. +3 more

A frequency analysis of the short-period modulation of the GCR as seen by instruments aboard Ulysses shows interesting temporal variations. In particular, during an approximate five-month period from December 1993 to May 1994, the modulation was not the usual 26 days but more than 29 days. The CIR-associated MeV ions did not exhibit this period sh…

1997 Geophysical Research Letters
Ulysses 6
The Latitudinal Structure of the Solar Wind in the Vicinity of the Solar Equator near Solar Minimum: 1986 and Predictions for 1997
DOI: 10.1029/97GL00540 Bibcode: 1997GeoRL..24..627G

Gazis, P. R.

In situ observations by different spacecraft have shown that the heliospheric current sheet (HCS) is associated with a narrow band of low speed high density solar wind. The inclination of the HCS and the three-dimensional structure of solar wind streams is related to the inclination of the coronal neutral line. Observations from the Ulysses spacec…

1997 Geophysical Research Letters
Ulysses 6