TY - JOUR
T1 - Ulysses observations of very different heliospheric structure during the declining phase of solar activity cycle 23
AU - McComas, D. J.
AU - Elliott, H. A.
AU - Gosling, J. T.
AU - Skoug, R. M.
PY - 2006/5/16
Y1 - 2006/5/16
N2 - This study examines the most recent observations from the solar wind experiment (SWOOPS) on the Ulysses spacecraft. In contrast to observations over the same locations in the declining phase of the previous solar activity cycle, these data show a more complicated heliospheric structure. Around the start of 2003, a band of slow solar wind resided at ∼20°-25°N latitude at all heliolongitudes. Subsequently, Ulysses failed to observe a well-organized corotating stream structure as it headed southward from the ecliptic plane, even though, in the previous solar cycle, Ulysses observed a regularly structured stream pattern. These observations show that the three-dimensional structure of the heliosphere can differ significantly from one solar cycle to the next. Finally, we show that the solar wind dynamic pressure has been relatively stable throughout 2005, indicating that the termination shock distance will also likely be relatively stable throughout 2006.
AB - This study examines the most recent observations from the solar wind experiment (SWOOPS) on the Ulysses spacecraft. In contrast to observations over the same locations in the declining phase of the previous solar activity cycle, these data show a more complicated heliospheric structure. Around the start of 2003, a band of slow solar wind resided at ∼20°-25°N latitude at all heliolongitudes. Subsequently, Ulysses failed to observe a well-organized corotating stream structure as it headed southward from the ecliptic plane, even though, in the previous solar cycle, Ulysses observed a regularly structured stream pattern. These observations show that the three-dimensional structure of the heliosphere can differ significantly from one solar cycle to the next. Finally, we show that the solar wind dynamic pressure has been relatively stable throughout 2005, indicating that the termination shock distance will also likely be relatively stable throughout 2006.
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U2 - 10.1029/2006GL025915
DO - 10.1029/2006GL025915
M3 - Article
AN - SCOPUS:33745685127
SN - 0094-8276
VL - 33
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 9
M1 - L09102
ER -