Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/7057
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dc.contributor.authorPant, V-
dc.contributor.authorMazumder, R-
dc.contributor.authorYuan, Ding-
dc.contributor.authorBanerjee, D-
dc.contributor.authorSrivastava, A. K-
dc.contributor.authorShen, Yuandeng-
dc.date.accessioned2020-11-17T11:54:22Z-
dc.date.available2020-11-17T11:54:22Z-
dc.date.issued2016-11-
dc.identifier.citationSolar Physics, Vol. 291, No. 11, pp. 3303-3315en_US
dc.identifier.issn1573-093X-
dc.identifier.urihttp://prints.iiap.res.in/handle/2248/7057-
dc.descriptionRestricted Access © Springer The original publication is available at springerlink.com http://dx.doi.org/10.1007/s11207-016-1018-7en_US
dc.description.abstractWe report on the co-existence of longitudinal and transverse oscillations in an active-region filament. On March 15, 2013, an M1.1 class flare was observed in Active Region AR 11692. A coronal mass ejection (CME) was found to be associated with the flare. The CME generated a shock wave that triggered the oscillations in a nearby filament, situated south-west of the active region as observed from National Solar Observatory (NSO) Global Oscillation Network Group (GONG) Hα images. In this work we report the longitudinal oscillations in the two ends of the filament, which co-existed with the transverse oscillations. We propose a scenario in which an incoming shock wave hits the filament obliquely and triggers both longitudinal and transverse oscillations. Using the observed parameters, we estimate the lower limit of the magnetic field strength. We use a simple pendulum model with gravity as the restoring force to estimate the radius of curvature. We also calculate the mass accretion rate that causes the filament motions to damp quite fast.en_US
dc.language.isoenen_US
dc.publisherSpringeren_US
dc.subjectSun, oscillationen_US
dc.subjectSun, filamenten_US
dc.subjectSun, magnetic fielden_US
dc.titleSimultaneous longitudinal and transverse oscillations in an active-region filamenten_US
dc.typeArticleen_US
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