We present a comprehensive spectro-temporal analysis of GRS observed with AstroSat during June, . A detailed study of the temporal properties reveals the appearance of an unknown' variability class ($τ$) during $ρ\rightarrow κ$ class transition of the source. This new unknown’ class () is characterized by the irregular repetition of low count dips' along with the adjacent flare’ like features in between two successive steady count rate durations, resulting in uniform $C$' shaped distribution in the color-color diagram. A detailed comparative study of the variability properties between the $τ$ class and other known variability classes of GRS $1915+105$ indicates it as a distinct variability class of the source. Further, we find evidence of the presence of possible HFQPO features at $\sim 71$ Hz with quality factor $\sim 13$, rms amplitude $\sim 4.69\%$, and significance $3σ$, respectively. In addition, a harmonic-like feature at $\sim 152$ Hz is also seen with quality factor $\sim 21$, rms amplitude $\sim 5.75\%$ and significance $\sim 4.7σ$. The energy-dependent power spectral study reveals that the fundamental HFQPO and its harmonic are present in $3-15$ keV and $3-6$ keV energy ranges, respectively. Moreover, the wide-band ($0.7-50$ keV) spectral modelling comprising of thermal Comptonization component indicates the presence of a cool ($kT_{\rm e}\sim 1.7$ keV) and optically thick (optical depth $\sim 14$) Comptonizing corona’, which seems to be responsible in regulating the HFQPO features in GRS +. Finally, we find the bolometric luminosity () to be about within keV, indicating the sub-Eddington accretion regime of the source.

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