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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
Detection of SO2 on Callisto with the Hubble Space Telescope
DOI: 10.1029/97GL00876 Bibcode: 1997GeoRL..24.1139N

Johnson, Robert E.; McGrath, Melissa A.; Noll, Keith S. +1 more

We have detected SO2 in ultraviolet spectra of Callisto obtained with the Hubble Space Telescope's Faint Object Spectrograph. An absorption band centered at 280 nm appears in the spectrum of Callisto's leading hemisphere, but is not apparent in the spectrum of the trailing hemisphere. The band is similar to the SO2 band on Eu…

1997 Geophysical Research Letters
eHST 47
The Pele Plume (Io): Observations with the Hubble Space Telescope
DOI: 10.1029/97GL02592 Bibcode: 1997GeoRL..24.2471S

Ballester, Gilda E.; McGrath, Melissa A.; Spencer, John R. +3 more

In July 1996, with the Hubble Space Telescope (HST), we observed the Pele plume silhouetted against Jupiter at a wavelength of 0.27µm, the first definitive observation of an Io plume from Earth. The height, 420 ± 40 km, was greater than any plume observed by Voyager. The plume had significantly smaller optical depth at 0.34 and 0.41µm, where it wa…

1997 Geophysical Research Letters
eHST 47
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
Venus tail ray observation near Earth
DOI: 10.1029/97GL01159 Bibcode: 1997GeoRL..24.1163G

Livi, S.; Hsieh, K. C.; Wurz, P. +23 more

In June, 1996, Venus passed through a very close inferior conjunction with the Sun. At that time the CTOF detector of the CELIAS mass spectrometer experiment on the SOHO spacecraft near Earth's L1 Lagrangian point was measuring heavy ions in the solar wind ∼4.5 × 107 km downstream of Venus. Close to the time predicted by simple geometri…

1997 Geophysical Research Letters
SOHO 31
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
Is the geoeffectiveness of the 6 January 1997 CME predictable from solar observations?
DOI: 10.1029/97GL03000 Bibcode: 1997GeoRL..24.2965Z

Hoeksema, J. T.; Zhao, X. P.

We present a prediction scheme for specifying the duration and maximum strength of the southward IMF within a magnetic cloud from observations of the disappearing filament associated with the coronal mass ejection and the photospheric magnetic field made near the filament disappearing. Using this scheme we were able to predict that the Earth direc…

1997 Geophysical Research Letters
SOHO 25
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