摘要: We report on observations of highly-varying Si IV 1402.77 line profiles
observed with the Interface Region Imaging Spectrograph (IRIS) during the
M-class flare from 2022 January 18 at an unprecedented 0.8 s cadence. Moment
analysis of this line observed in flare ribbon kernels showed that the
intensity, Doppler velocity, and non-thermal broadening exhibited variations
with periods below 10 s. These variations were found to be correlated with
properties of the Gaussian fit to a well-resolved secondary component of the
line redshifted by up to 70 km s$^{-1}$, while the primary component was
consistently observed near the rest wavelength of the line. A particularly high
correlation was found between the non-thermal broadening of the line resulting
from the moment analysis and the redshift of the secondary component. This
means that the oscillatory enhancements in the line broadening were due to
plasma flows (away from the observer) with varying properties. A simple
de-projection of the Doppler velocities of the secondary component based on a
three-dimensional reconstruction of flare loops rooted in the kernel suggests
that the observed flows were caused by downflows and compatible with strong
condensation flows recently predicted by numerical simulations. Furthermore,
peaks of the intensity and the trends of Doppler velocity of the Gaussian fit
to the secondary component (averaged in the ribbon) were found to correspond to
one of the quasi-periodic pulsations (QPPs) detected during the event in the
soft X-ray flux (as measured by the Geostationary Operational Environmental
Satellite, GOES) and the microwave radio flux (as measured by the Expanded
Owens Valley Solar Array, EOVSA). This result supports a scenario in which the
QPPs were driven by repeated magnetic reconnection.