Direct Detection of a Coronal Mass Ejection–Associated Shock in Large Angle and Spectrometric Coronagraph Experiment White‐Light Images

2003 ◽  
Vol 598 (2) ◽  
pp. 1392-1402 ◽  
Author(s):  
A. Vourlidas ◽  
S. T. Wu ◽  
A. H. Wang ◽  
P. Subramanian ◽  
R. A. Howard
2020 ◽  
Vol 899 (1) ◽  
pp. 12
Author(s):  
Beili Ying ◽  
Alessandro Bemporad ◽  
Li Feng ◽  
Lei Lu ◽  
Weiqun Gan ◽  
...  

2009 ◽  
Vol 705 (1) ◽  
pp. 426-435 ◽  
Author(s):  
Vasyl Yurchyshyn ◽  
Valentyna Abramenko ◽  
Durgesh Tripathi

2017 ◽  
Vol 7 ◽  
pp. A2 ◽  
Author(s):  
Carolina Salas Matamoros ◽  
Karl Ludwig Klein ◽  
Gerard Trottet

The propagation of a coronal mass ejection (CME) to the Earth takes between about 15 h and several days. We explore whether observations of non-thermal microwave bursts, produced by near-relativistic electons via the gyrosynchrotron process, can be used to predict travel times of interplanetary coronal mass ejections (ICMEs) from the Sun to the Earth. In a first step, a relationship is established between the CME speed measured by the Solar and Heliospheric Observatory/Large Angle and Spectrometric Coronagraph (SoHO/LASCO) near the solar limb and the fluence of the microwave burst. This relationship is then employed to estimate speeds in the corona of earthward-propagating CMEs. These speeds are fed into a simple empirical interplanetary acceleration model to predict the speed and arrival time of the ICMEs at Earth. The predictions are compared with observed arrival times and with the predictions based on other proxies, including soft X-rays (SXR) and coronographic measurements. We found that CME speeds estimated from microwaves and SXR predict the ICME arrival at the Earth with absolute errors of 11 ± 7 and 9 ± 7 h, respectively. A trend to underestimate the interplanetary travel times of ICMEs was noted for both techniques. This is consistent with the fact that in most cases of our test sample, ICMEs are detected on their flanks. Although this preliminary validation was carried out on a rather small sample of events (11), we conclude that microwave proxies can provide early estimates of ICME arrivals and ICME speeds in the interplanetary space. This method is limited by the fact that not all CMEs are accompanied by non-thermal microwave bursts. But its usefulness is enhanced by the relatively simple observational setup and the observation from ground, which makes the instrumentation less vulnerable to space weather hazards.


Solar Physics ◽  
2016 ◽  
Vol 291 (5) ◽  
pp. 1405-1416 ◽  
Author(s):  
K. Hariharan ◽  
R. Ramesh ◽  
C. Kathiravan ◽  
T. J. Wang

2008 ◽  
Vol 26 (10) ◽  
pp. 3067-3075 ◽  
Author(s):  
G. Poletto ◽  
A. Bemporad ◽  
F. Landini ◽  
M. Romoli

Abstract. This paper aims at studying reconnection occurring in the aftermath of the 28 May 2004, CME, first imaged by the LASCO (Large Angle and Spectrometric Coronagraph) C2 at 11:06 UT. The CME was observed in White Light and UV radiation: images acquired by the LASCO C2 and C3 coronagraphs and spectra acquired by UVCS (Ultraviolet Coronagraph Spectrometer) allowed us to identify the level at which field lines, stretched outwards by the CME ejection, reconnect below the CME bubble. As the CME propagates outwards, reconnection occurs at increasingly higher levels. The process goes on at a low pace for several hours: here we give the profile of the reconnection rate vs. heliocentric distance over a time interval of ≈14 h after the CME onset, extending estimates of the reconnection rate to larger distances than previously inferred by other authors. The reconnection rate appears to decrease with time/altitude. We also calculate upper and lower limits to the density in the diffusion region between 4 and 7 R⊙ and conclude by comparing estimates of the classical and anomalous resistivity in the diffusion region with the value inferred from the data. The latter turns out to be ≥5 order of magnitudes larger than predicted by classical or anomalous theories, pointing to the need of identifying the process responsible for the observed value.


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