Matches in SemOpenAlex for { <https://semopenalex.org/work/W3099515877> ?p ?o ?g. }
- W3099515877 endingPage "16" @default.
- W3099515877 startingPage "16" @default.
- W3099515877 abstract "We investigate the footpoints of four erupted magnetic flux ropes (MFRs) that appear as sigmoidal hot channels prior to the eruptions in the Atmospheric Imaging Assembly high temperaure passbands. The simultaneous Helioseismic and Magnetic Imager observations disclose that one footpoint of the MFRs originates in the penumbra or penumbra edge with a stronger magnetic field, while the other in the moss region with a weaker magnetic field. The significant deviation of the axis of the MFRs from the main polarity inversion lines and associated filaments suggests that the MFRs have ascended to a high altitude, thus being distinguishable from the source sigmoidal ARs. The more interesting thing is that, with the eruption of the MFRs, the average inclination angle and direct current at the footpoints with stronger magnetic field tend to decrease, which is suggestive of a straightening and untwisting of the magnetic field in the MFR legs. Moreover, the associated flare ribbons also display an interesting evolution. They initially appear as sporadical brightenings at the two footpoints of and in the regions below the MFRs and then quickly extend to two slender sheared J-shaped ribbons with the two hooks corresponding to the two ends of the MFRs. Finally, the straight parts of the two ribbons separate from each other, evolving into two widened parallel ones. These features mostly conforms to and supports the recently proposed three-dimensional standard CME/flare model, i.e., the twisted MFR eruption stretches and leads to the reconnection of the overlying field that transits from a strong to weak shear with the increasing height." @default.
- W3099515877 created "2020-11-23" @default.
- W3099515877 creator A5000460407 @default.
- W3099515877 creator A5040109851 @default.
- W3099515877 date "2016-07-26" @default.
- W3099515877 modified "2023-10-18" @default.
- W3099515877 title "THE CHARACTERISTICS OF THE FOOTPOINTS OF SOLAR MAGNETIC FLUX ROPES DURING ERUPTIONS" @default.
- W3099515877 cites W1510126286 @default.
- W3099515877 cites W1845885259 @default.
- W3099515877 cites W1969100534 @default.
- W3099515877 cites W1969115216 @default.
- W3099515877 cites W1969354548 @default.
- W3099515877 cites W1972119866 @default.
- W3099515877 cites W1973482511 @default.
- W3099515877 cites W1973792090 @default.
- W3099515877 cites W1982578430 @default.
- W3099515877 cites W1987089087 @default.
- W3099515877 cites W1987804400 @default.
- W3099515877 cites W1988186292 @default.
- W3099515877 cites W1991677485 @default.
- W3099515877 cites W1992902329 @default.
- W3099515877 cites W1993024572 @default.
- W3099515877 cites W1994075064 @default.
- W3099515877 cites W1996315656 @default.
- W3099515877 cites W1999363600 @default.
- W3099515877 cites W1999527160 @default.
- W3099515877 cites W1999696263 @default.
- W3099515877 cites W2005574947 @default.
- W3099515877 cites W2006130429 @default.
- W3099515877 cites W2006240613 @default.
- W3099515877 cites W2008888110 @default.
- W3099515877 cites W2009458073 @default.
- W3099515877 cites W2011493562 @default.
- W3099515877 cites W2011781064 @default.
- W3099515877 cites W2012136927 @default.
- W3099515877 cites W2013602603 @default.
- W3099515877 cites W2014209718 @default.
- W3099515877 cites W2015069526 @default.
- W3099515877 cites W2018405851 @default.
- W3099515877 cites W2024401613 @default.
- W3099515877 cites W2025304472 @default.
- W3099515877 cites W2025419326 @default.
- W3099515877 cites W2027318245 @default.
- W3099515877 cites W2027332074 @default.
- W3099515877 cites W2027837530 @default.
- W3099515877 cites W2030384010 @default.
- W3099515877 cites W2030493213 @default.
- W3099515877 cites W2031510649 @default.
- W3099515877 cites W2032102567 @default.
- W3099515877 cites W2036301863 @default.
- W3099515877 cites W2038115604 @default.
- W3099515877 cites W2038957915 @default.
- W3099515877 cites W2040219663 @default.
- W3099515877 cites W2040960936 @default.
- W3099515877 cites W2042765690 @default.
- W3099515877 cites W2046195076 @default.
- W3099515877 cites W2047634950 @default.
- W3099515877 cites W2048465377 @default.
- W3099515877 cites W2051945869 @default.
- W3099515877 cites W2056890589 @default.
- W3099515877 cites W2061062646 @default.
- W3099515877 cites W2070034514 @default.
- W3099515877 cites W2072668462 @default.
- W3099515877 cites W2083583224 @default.
- W3099515877 cites W2088959242 @default.
- W3099515877 cites W2089467007 @default.
- W3099515877 cites W2094483427 @default.
- W3099515877 cites W2094915848 @default.
- W3099515877 cites W2100400062 @default.
- W3099515877 cites W2102570751 @default.
- W3099515877 cites W2108882534 @default.
- W3099515877 cites W2109526506 @default.
- W3099515877 cites W2109836133 @default.
- W3099515877 cites W2117294031 @default.
- W3099515877 cites W2122755404 @default.
- W3099515877 cites W2126965136 @default.
- W3099515877 cites W2138331031 @default.
- W3099515877 cites W2141665517 @default.
- W3099515877 cites W2142234851 @default.
- W3099515877 cites W2153097002 @default.
- W3099515877 cites W2158612941 @default.
- W3099515877 cites W2161975006 @default.
- W3099515877 cites W2170756090 @default.
- W3099515877 cites W2171364494 @default.
- W3099515877 cites W2230176024 @default.
- W3099515877 cites W2363018612 @default.
- W3099515877 cites W2461520053 @default.
- W3099515877 cites W2963177646 @default.
- W3099515877 cites W3098368535 @default.
- W3099515877 cites W3098735175 @default.
- W3099515877 cites W3099151694 @default.
- W3099515877 cites W3099658297 @default.
- W3099515877 cites W3099707401 @default.
- W3099515877 cites W3100570562 @default.
- W3099515877 cites W3100711836 @default.
- W3099515877 cites W3100929025 @default.
- W3099515877 cites W3101052731 @default.
- W3099515877 cites W3101553904 @default.