摘要: Solar filaments exist as stable structures for extended periods of time
before many of them form the core of a CME. We examine the properties of an
erupting filament on 2017 May 29--30 with high-resolution He I 10830 A and
Halpha spectra from the Dunn Solar Telescope, full-disk Dopplergrams of He I
10830 A from the Chromospheric Telescope, and EUV and coronograph data from SDO
and STEREO. Pre-eruption line-of-sight velocities from an inversion of He I
with the HAZEL code exhibit coherent patches of 5 Mm extent that indicate
counter-streaming and/or buoyant behavior. During the eruption, individual,
aligned threads appear in the He I velocity maps. The distribution of
velocities evolves from Gaussian to strongly asymmetric. The maximal optical
depth of He I 10830 A decreased from tau = 1.75 to 0.25, the temperature
increased by 13 kK, and the average speed and width of the filament increased
from 0 to 25 km s-1 and 10 to 20 Mm, respectively. All data sources agree that
the filament rose with an exponential acceleration reaching 7.4 m s-2 that
increased to a final velocity of 430 km s-1 at 22:24 UT; a CME was associated
with this filament eruption. The properties during the eruption favor a
kink/torus instability, which requires the existence of a flux rope. We
conclude that full-disk chromospheric Dopplergrams can be used to trace the
initial phase of on-disk filament eruptions in real-time, which might
potentially be useful for modelling the source of any subsequent CMEs.