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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 111,
A07S14,
doi:10.1029/2005JA011394,
2006
The 17–22 October (1999) solar-interplanetary-geomagnetic event: Very intense geomagnetic storm associated with a pressure
balance between interplanetary coronal mass ejection and a high-speed stream
Alisson Dal Lago
Instituto Nacional de Pesquisas Espaciais, São José dos Campos, São Paulo, Brazil
Walter D. Gonzalez
Instituto Nacional de Pesquisas Espaciais, São José dos Campos, São Paulo, Brazil
Laura A. Balmaceda
Max-Planck-Institut für Sonnensystemforschung, Katlenburg-Lindau, Germany
Luis E. A. Vieira
Instituto Nacional de Pesquisas Espaciais, São José dos Campos, São Paulo, Brazil
Ezequiel Echer
Instituto Nacional de Pesquisas Espaciais, São José dos Campos, São Paulo, Brazil
Fernando L. Guarnieri
Instituto Nacional de Pesquisas Espaciais, São José dos Campos, São Paulo, Brazil
Jean Santos
Max-Planck-Institut für Sonnensystemforschung, Katlenburg-Lindau, Germany
Marlos R. da Silva
Instituto Nacional de Pesquisas Espaciais, São José dos Campos, São Paulo, Brazil
Aline de Lucas
Instituto Nacional de Pesquisas Espaciais, São José dos Campos, São Paulo, Brazil
Alicia L. Clua de Gonzalez
Instituto Nacional de Pesquisas Espaciais, São José dos Campos, São Paulo, Brazil
Ranier Schwenn
Max-Planck-Institut für Sonnensystemforschung, Katlenburg-Lindau, Germany
Nelson J. Schuch
Centro Regional Sul de Pesquisas Espaciais, Santa Maria, Rio Grande do Sol, Brazil
Abstract
Using observations from the Advanced Composition Explorer (ACE) magnetic field and plasma experiments, we investigate the
magnetic, thermal, and dynamic pressure balance in the border of a high-speed stream (HSS) and an average-speed interplanetary
coronal mass ejection (ICME) observed on 21–22 October (1999). We believe that the HSS compressed the ICME and intensified
its internal southward magnetic field, resulting in a very intense geomagnetic storm, with peak Dst of −237 nT. In solar cycle
23 this was the only event, out of 18 very intense geomagnetic storms, i.e., peak Dst < −200 nT, which was caused by such
a mechanism. We also address the solar origin of this very intense geomagnetic storm, using combined solar data from three
different sources: a ground-based source, coronal hole maps from the National Solar Observatory (NSO) at Kitt Peak, and two
satellite-based sources, eruption activity from the Extreme Ultraviolet Imaging Telescope (EIT) and coronal mass ejection
observations from the Large Angle and Spectrometric Coronagraph (LASCO), both aboard the Solar and Heliospheric Observatory
(SOHO). A coronal hole is evident just beside (to the east of) the active region from which an average-speed coronal mass
ejection lifted off on 17–18 October (1999). This was the only possible solar origin of the 21–22 October interplanetary geomagnetic
event.
Received 31
August
2005;
accepted 28
March
2006;
published 22
June
2006.
Keywords: coronal mass ejections;
geomagnetic storms;
speed streams.
Index Terms: 2788 Magnetospheric Physics: Magnetic storms and substorms (7954); 7513 Solar Physics, Astrophysics, and Astronomy: Coronal mass ejections (2101); 7511 Solar Physics, Astrophysics, and Astronomy: Coronal holes; 2111 Interplanetary Physics: Ejecta, driver gases, and magnetic clouds; 2102 Interplanetary Physics: Corotating streams.
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Citation: Dal Lago, A., et al.
(2006),
The 17–22 October (1999) solar-interplanetary-geomagnetic event: Very intense geomagnetic storm associated with a pressure
balance between interplanetary coronal mass ejection and a high-speed stream,
J. Geophys. Res.,
111,
A07S14,
doi:10.1029/2005JA011394.
Copyright 2006 by the American Geophysical Union.
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