1997
DOI: 10.1023/a:1004943213433
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Cited by 169 publications
(112 citation statements)
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“…Such a stability suggests that the charge state composition measured during the 1994-1996 pass may be very similar to the one corresponding to the SUMER observations so that the Ulysses measurements can be combined to the SUMER observations despite the fact that the former took place earlier. Thus, we will restrict our comparison to the data taken in 1994-1996. Measurements from the 1994-1996 pass were published by Ko et al (1997), von Steiger et al (2000, and Gloeckler & Geiss (2007). The differences between these studies consist mainly of the time interval that each of them considered, whether they discriminated between the south and north polar wind or not, and what elements they studied.…”
Section: Ulysses Composition Measurementsmentioning
confidence: 99%
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“…Such a stability suggests that the charge state composition measured during the 1994-1996 pass may be very similar to the one corresponding to the SUMER observations so that the Ulysses measurements can be combined to the SUMER observations despite the fact that the former took place earlier. Thus, we will restrict our comparison to the data taken in 1994-1996. Measurements from the 1994-1996 pass were published by Ko et al (1997), von Steiger et al (2000, and Gloeckler & Geiss (2007). The differences between these studies consist mainly of the time interval that each of them considered, whether they discriminated between the south and north polar wind or not, and what elements they studied.…”
Section: Ulysses Composition Measurementsmentioning
confidence: 99%
“…The differences between these studies consist mainly of the time interval that each of them considered, whether they discriminated between the south and north polar wind or not, and what elements they studied. Ko et al (1997) averaged a 100 day set of data taken from day 170 to 270 in 1994, during the Ulysses pass over the south pole, and measured the charge state Ko et al 1997); those for the north pole were averaged from day 182 of 1995 to day 121 of 1996, and represent the data set closest in time to the SUMER observations. The south pole composition was slightly but significantly shifted toward higher charge states than the north pole one.…”
Section: Ulysses Composition Measurementsmentioning
confidence: 99%
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“…For instance, Ko et al (1997) obtained a temperature of ≈1.5 MK at 1.4 R . Attempts to reconcile the observations with their interpretations were made by assuming differential flows between ions of the same element (Esser and Edgar 2001), but recent studies conclude that non-Maxwellian electron velocity distributions with an enhanced supra-thermal tail are required in the inner corona to account for the observed charge distributions in the solar wind (Chen et al 2003).…”
Section: The Thermal Structurementioning
confidence: 99%