2016
DOI: 10.1002/2015ja021615
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A data‐constrained three‐dimensional magnetohydrodynamic simulation model for a coronal mass ejection initiation

Abstract: In this study, we present a three‐dimensional magnetohydrodynamic model based on an observed eruptive twisted flux rope (sigmoid) deduced from solar vector magnetograms. This model is a combination of our two very well tested MHD models: (i) data‐driven 3‐D magnetohydrodynamic (MHD) active region evolution (MHD‐DARE) model for the reconstruction of the observed flux rope and (ii) 3‐D MHD global coronal‐heliosphere evolution (MHD‐GCHE) model to track the propagation of the observed flux rope. The 6 September 20… Show more

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Cited by 13 publications
(6 citation statements)
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“…In summary, a data-driven MHD modelling like the one shown here, which is able to realistically simulate the whole process from origin to onset of a solar eruption, can be used as a new way for studying the cause of solar eruptions. Furthermore, utilizing the output of such realistic model as the CME initiation input for models of solar storms travelling from the Sun to Earth 57 58 59 will be, we believe, a step forward in developing sophisticated modelling for space weather.…”
Section: Discussionmentioning
confidence: 99%
“…In summary, a data-driven MHD modelling like the one shown here, which is able to realistically simulate the whole process from origin to onset of a solar eruption, can be used as a new way for studying the cause of solar eruptions. Furthermore, utilizing the output of such realistic model as the CME initiation input for models of solar storms travelling from the Sun to Earth 57 58 59 will be, we believe, a step forward in developing sophisticated modelling for space weather.…”
Section: Discussionmentioning
confidence: 99%
“…We conclude that solar wind modeling tools can be used to provide solar wind context at Mars' orbital location for planetary studies. Although this study focused on the WSA‐ENLIL + Cone model, other solar wind models [e.g., Hakamada and Akasofu , ; Tóth et al ., ; Hayashi , ; Feng et al ., , , ; Wu et al ., ; Yang et al ., , ; Liou et al ., ; Intriligator et al ., ; Wu et al ., ] could also be utilized to provide continuous upstream conditions at Mars. A particular advantage of the continuous conditions provided by models is that they can be used to fill any data gaps in in situ observations.…”
Section: Discussionmentioning
confidence: 99%
“…Modeling of continuous solar wind conditions throughout the inner heliosphere continues to advance in capability and accuracy [e.g., Pizzo et al, 2011;Tóth et al, 2012;Lee et al, 2013;Intriligator et al, 2015a;Wu et al, 2016aWu et al, , 2016b and has been applied to study solar wind-body interactions [e.g., Baker et al, 2013;Dewey et al, 2015]. While many solar wind models exist [e.g., Hakamada and Akasofu, 1982;Tóth et al, 2005;Hayashi, 2012;Feng et al, 2011Feng et al, , 2012Feng et al, , 2014Yang et al, 2011Yang et al, , 2012Liou et al, 2014;Intriligator et al, 2015b;Wu et al, 2016], here we present upstream solar wind conditions at Mars modeled by the Wang-Sheeley-Arge (WSA)-ENLIL + Cone model over the period from late November 2014 to mid-March 2015. This period corresponds to the beginning of the science mapping phase of the Mars Atmosphere and Volatile Evolution (MAVEN) spacecraft until its last observations of the pristine upstream solar wind for several months due to its orbit.…”
Section: Introductionmentioning
confidence: 99%
“…An immediate approach is to parameterize the relationship functions and seek a set of optimal parameters for each solar rotation period and express them as functions of time, or other relevant parameters, such as magnetic field strength or proxy of coronal magnetic field structure, in addition to flow speed. Furthermore, such improved relation functions can represent the state of solar wind plasma near the Sun that cannot be well measured with remote sensing technique or space probes today; therefore, the modified functions can offer a good constraint or requirement to models of coronal heating and accelerations [e.g., Usmanov et al, 2000Usmanov et al, , 2011Yang et al, 2016] and enhance MHD simulation models for the trans-Alfvenic solar corona [e.g., Hayashi, 2005;Feng et al, 2010;Riley et al, 2011;Yang et al, 2012;Feng et al, 2012Feng et al, , 2015Wu et al, 2016] and interplanetary space [e.g., Dryer, 1994;Wu et al, 2005;Kataoka et al, 2009;Odstrcil and Pizzo, 2009;Intriligator et al, 2010;Detman et al, 2011;Wu et al, 2011;Hayashi, 2012;Kim et al, 2014] and heliospheric models [e.g., Washimi et al, 2011;Pogorelov et al, 2013].…”
Section: Introductionmentioning
confidence: 99%