摘要: Lower atmospheric lines show peculiar profiles at the leading edge of ribbons
during solar flares. In particular, increased absorption of the BBSO/GST
\hei~10830~\AA\ line \citep[e.g.][]{Xu2016}, as well as broad and centrally
reversed profiles in the spectra of the \mgii~and \cii~lines observed by the
\iris~satellite \citep[e.g.][]{Panos2018,Panos2021a} have been reported. In
this work, we aim to understand the physical origin of the \iris\ ribbon front
line profiles, which seem to be common of many, if not all, flares. To achieve
this, we quantify the spectral properties of the \iris~\mgii~ribbon front
profiles during four large flares and perform a detailed comparison with a grid
of radiative hydrodynamic models using the \radynfp~code. We also studied their
transition region counterparts, finding that these ribbon front locations are
regions where transition region emission and chromospheric evaporation are
considerably weaker compared to other parts of the ribbons. Based on our
comparison between the \iris~observations and modelling, our interpretation is
that there are different heating regimes at play in the leading and trailing
regions of the ribbons. More specifically, we suggest that bombardment of the
chromosphere by more gradual and modest non-thermal electron energy fluxes can
qualitatively explain the \iris~observations at the ribbon front, while
stronger and more impulsive energy fluxes are required to drive chromospheric
evaporation and more intense TR emission. Our results provide a possible
physical origin for the peculiar behaviour of the \iris~chromospheric lines in
the ribbon leading edge and new constraints for the flare models.