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(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

High Speed Stream Properties and Related Geomagnetic Activity During the Whole Heliosphere Interval (WHI): 20 March to 16 April 2008

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Echer, E. [1] ; Tsurutani, B. T. [1, 2] ; Gonzalez, W. D. [1] ; Kozyra, J. U. [3]
Total Authors: 4
[1] Natl Inst Space Res INPE, Sao Jose Dos Campos, SP - Brazil
[2] CALTECH, Jet Prop Lab, Pasadena, CA - USA
[3] Univ Michigan, Ann Arbor, MI 48109 - USA
Total Affiliations: 3
Document type: Journal article
Source: SOLAR PHYSICS; v. 274, n. 1-2, p. 303-320, DEC 2011.
Web of Science Citations: 20

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 (a parts per thousand 3 -aEuro parts per thousand 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 -aEuro parts per thousand 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 -aEuro parts per thousand 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 a parts per thousand aEuro parts per thousand 30 nT(2) and < 10 nT(2) in the high speed streams proper. (AU)

FAPESP's process: 08/06650-9 - Study of geoeffective interplanetary structures during intense geomagnetic storms and substorms
Grantee:Walter Demetrio Gonzalez Alarcon
Support Opportunities: Regular Research Grants