@Article{EcherTsurGonzKozy:2011:20Ma16,
author = "Echer, E. and Tsurutani, Bruce T and Gonzalez, Walter Demetrio and
Kozyra, J.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and Jet
Propulsion Laboratory, California Institute of Technology and
{Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "High Speed Stream Properties and Related Geomagnetic Activity
During the Whole Heliosphere Interval (WHI): 20 March to 16 April
2008",
journal = "Solar Physics",
year = "2011",
volume = "xx",
month = "Mar.",
keywords = "Solar wind, High-speed streams, Geomagnetic activity, Solar cycle,
Space weather, Whole heliosphere interval, Alfv¨¦n waves, Nested
variances.",
abstract = "We study the interplanetary features and concomitant geomagnetic
activity of the two high-speed streams (HSSs) selected by the
Whole Heliosphere Interval (WHI) campaign participants: 20 March
to 16 April 2008 in Carrington rotation (CR) 2068. This interval
was chosen to perform a comprehensive study of HSSs and their
geoeffectiveness during this {"}deep{"} solar minimum. The two
HSSs within the interval were characterized by fast solar-wind
speeds (peak values > 600 km s-1) containing large-amplitude
Alfv¨¦nic fluctuations, as is typical of HSSs during normal solar
minima. However, the interplanetary magnetic field (IMF) magnitude
[B o] was exceptionally low (¡{\"O}3 - 5 nT) during these HSSs,
leading to lower than usual IMF B z values. The first HSS (HSS1)
had favorable IMF polarity for geomagnetic activity (negative
during northern Spring). The average AE and Dst for the HSS1
proper (HSS1P) were + 258 nT and - 21 nT, respectively. The second
HSS (HSS2) had a positive sector IMF polarity, one that is less
favorable for geomagnetic activity. The AE and Dst index averages
were + 188 nT and - 7 nT, both lower than corresponding numbers
for the first event, as expected. The HSS1P geomagnetic activity
is comparable to, and the HSS2P geomagnetic activity lower than,
corresponding observations for the previous minimum (1996). Both
events' geomagnetic activities are lower than HSS events
previously studied in the declining phase (in 2003). In general, V
sw was faster for the HSSs in 2008 compared to 1996. The southward
IMF B z was lower in the former. The product of these two
parameters [V sw and IMF B z ] comprises the solar-wind electric
field, which is most directly associated with the energy input
into the magnetosphere during the HSS intervals. Thus the combined
effects led to the solar wind energy input in 2008 being slightly
less than that in 1996. A detailed analysis of magnetic-field
variances and Alfv¨¦nicity is performed to explore the
characteristics of Alfv¨¦n waves (a central element in the
geoeffectiveness of HSSs) during the WHI. The B z variances in the
proto-CIR (PCIR) were ¡{\"O} 30 nT2 and < 10 nT2 in the high
speed streams proper.",
doi = "10.1007/s11207-011-9739-0",
url = "http://dx.doi.org/10.1007/s11207-011-9739-0",
issn = "0038-0938 and 1573-093X",
language = "en",
urlaccessdate = "29 jun. 2024"
}