One-third of the net power put in the ocean comes from internal tides that form due to the gravitational pull of the Sun, the Moon, and other celestial objects. These internal tides exchange energy with other internal waves, and slowly-evolving balanced eddies. Such energy interactions at large mesoscales differ considerably from those at smaller submesocales. We investigate energy exchanges of internal tides with balanced flow across length scales. For low Rossby number flows at large mesoscales, tide-eddy interaction is weak, with eddies transferring energy to large scales, hence preserving their coherent structures. At high Rossby number submesocale flows, strong tide-eddy interactions break the large-scale eddies and increase turbulent flow cascade strengths. Such interactions not only generate waves with harmonics of the tidal frequency, but also energize rapidly evolving non-wave ageostrophic motions. This leads to an internal wave continuum formation. The intermediate and high Rossby number flows are also more efficient at transferring energy across scales, and a considerable amount of the energy flux responsible for such energy transfers comes from regions with low and intermediate relative vorticity and horizontal divergence. By quantifying pathways for energy exchanges across length and timescales, our study offers new insights into the energetics of baroclinic tides in the ocean.