Pregled bibliografske jedinice broj: 478834
Relative kinematics of the leading edge and the prominence in coronal mass ejection
Relative kinematics of the leading edge and the prominence in coronal mass ejection // IHY-ISWI Regional Meeting Heliophysical phenomena and Earth's environment
Šibenik, Hrvatska, 2009. (poster, nije recenziran, pp prezentacija, znanstveni)
CROSBI ID: 478834 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Relative kinematics of the leading edge and the prominence in coronal mass ejection
Autori
Maričić, Darije ; Vršnak, Bojan ; Roša, Dragan ; Romštajn, Ivan
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, pp prezentacija, znanstveni
Skup
IHY-ISWI Regional Meeting Heliophysical phenomena and Earth's environment
Mjesto i datum
Šibenik, Hrvatska, 07.09.2009. - 13.09.2009
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
Sun: coronal mass ejection (CMEs)
Sažetak
We present a statistical analysis of the relationship between the kinematics of the leading edge and the eruptive prominence in coronal mass ejections (CMEs). We study the acceleration phase of 18 CMEs in which kinematics was measured from the pre-eruption stage up to the post-acceleration phase. In all CMEs, the three part structure (the leading edge, the cavity, and the prominence) was clearly recognizable from early stages of the eruption. The data show a distinct correlation between the duration of the leading edge (LE) acceleration and eruptive prominence (EP) acceleration. In the majority of events (78%) the acceleration-phase onset of the LE is very closely synchronized (within ±20 min) with the acceleration of EP. However, in two events the LE acceleration started significantly earlier than the EP acceleration (> 50 min), and in two events the EP acceleration started earlier than the LE acceleration (> 40 min). The average peak-acceleration of LEs (281 ms−2) is about twice larger than the average peak-acceleration of EPs (136 ms−2). Our results for the first time quantitatively demonstrate what is the level of synchronization of the acceleration phase of LE and EP in a rather large sample of events, i.e., we quantify how often the eruption develops in a “self-similar" manner.
Izvorni jezik
Engleski
Znanstvena područja
Fizika
POVEZANOST RADA
Projekti:
007-0000000-1362 - Eruptivni procesi u Sunčevoj atmosferi
Ustanove:
Geodetski fakultet, Zagreb