2002
DOI: 10.5194/angeo-20-917-2002
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Arrival times of Flare/Halo CME associated shocks at the Earth: comparison of the predictions of three numerical models with these observations

Abstract: Abstract. The arrival times at L1 of eleven travelling shocks associated both with X-ray flaring and with halo CMEs recorded aboard SOHO/LASCO have been considered. Close to the Sun the velocities of these events were estimated using either Type II radio records or CME speeds. Close to the Earth the shocks were detected in the data of various solar wind plasma, interplanetary magnetic field (IMF) and energetic particle experiments aboard SOHO, ACE, WIND, INTERBALL-1 and IMP-8. The real-time shock arrival predi… Show more

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Cited by 39 publications
(39 citation statements)
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“…They are characterized by enhanced [N 2 ]/[O] and they propagate to lower latitudes carried by the horizontal neutral winds that arise from the pressure gradient force in the auroral oval and by ion drag in the polar cap. Then they cause negative storms by increasing the loss rate and decreasing the ionospheric electron density (see, e.g., Prölss, 1981Prölss, , 1993Buonsanto, 1999;Burns, Killeen, and Roble, 1991;Fuller-Rowell, Codrescu, and Araujo-Pradere, 2001). Feng and Zhao (2006) and Xie et al (2006) investigated the effect of HCS on propagation and geoeffectiveness of CME-ICME events and CME-IP shock events, respectively.…”
Section: Introductionmentioning
confidence: 97%
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“…They are characterized by enhanced [N 2 ]/[O] and they propagate to lower latitudes carried by the horizontal neutral winds that arise from the pressure gradient force in the auroral oval and by ion drag in the polar cap. Then they cause negative storms by increasing the loss rate and decreasing the ionospheric electron density (see, e.g., Prölss, 1981Prölss, , 1993Buonsanto, 1999;Burns, Killeen, and Roble, 1991;Fuller-Rowell, Codrescu, and Araujo-Pradere, 2001). Feng and Zhao (2006) and Xie et al (2006) investigated the effect of HCS on propagation and geoeffectiveness of CME-ICME events and CME-IP shock events, respectively.…”
Section: Introductionmentioning
confidence: 97%
“…Ionospheric storms are often described as positive storms when foF2 is increased and as negative storms when foF2 is significantly reduced. The negative storm is caused by changes in the atmospheric composition, and this explanation has been fully supported by analyzer measurements (Prölss, 1980). At the main phase of a magnetic storm, the enhanced energy input from the magnetosphere causes considerable heating of the ionized and neutral gases in the auroral zone, leading to the "composition bulges".…”
Section: Introductionmentioning
confidence: 98%
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“…, and references therein). These models include the "Shock Time of Arrival"/STOA Model (Dryer and Smart, 1984;Shea, 1984, 1985); the "Interplanetary Shock Propagation"/ISPM Model (Smith and Dryer, 1990); and the "Hakamada-Akasofu-Fry version 2"/modified HAFv.2 model Fry et al, 2001Fry et al, , 2003Fry et al, , 2004Fry et al, , 2005Fry et al, , 2007McKenna-Lawlor et al, 2002Sun et al, 2002aSun et al, , b, 2003. Overviews of the characteristics of these three models are provided in Sect.…”
Section: Predictive Modelsmentioning
confidence: 99%
“…The performances of the above three models have been tested and the comparative study revealed that the performances of these three models were practically identical in forecasting the shock arrival time (McKenna-Lawlor et al, 2002;Fry et al, 2003;Cho et al, 2003;McKenna-Lawlor et al, 2006).…”
Section: Introductionmentioning
confidence: 99%