Nitrogen-rich biomass pyrolysis has been explored as a green, distributed, and simple alternative for sustainable ammonia production at atmospheric pressure. In this paper, tea waste was selected as a promising feedstock, and H 2 was employed as an enhancer to increase the yield of NH 3 . The nitrogen distribution among three-phase pyrolytic products affected by various temperatures and different atmospheres was compared and discussed. The evolution pathways for fuel−N during tea waste pyrolysis under a H 2 -rich atmosphere were concluded. Results indicated that the introduction of H 2 was favorable for the increase of the gas− N yield but decreased the yields of char−N and tar−N. At lower temperatures, the bond cleavage of amide−N (N−A) in fuels was enhanced by H 2 , which then yielded more NH 3 −N through deamination. Subsequently, H 2 improved the production of nitrile−N in tar, as well as NH 3 −N and HCN−N, by accelerating the secondary cracking of amine−N (tar−N) generated from the decomposition of amide−N. However, the formation of heterocyclic−N in tar through the polymerization of amine−N was restrained under a H 2 -rich atmosphere. Pyrolysis in the presence of H 2 generated a large amount of H radicals. When the temperature continued to increase, sufficient H radicals impressively advanced the ring rupture (into HCN−N) and full hydrogenation (into NH 3 −N) of pyridinic−N/pyrrolic−N (N-6/N-5) in char. Meanwhile, H radicals also intensified the thermal cracking of nitrile−N and ring opening of heterocyclic−N to form more HCN−N and NH 3 −N. Overall, more nitrogen evolved into NH 3 −N and HCN−N during pyrolysis in a H 2 -rich atmosphere, especially at high temperatures. The highest NH 3 yield of 43.33 wt % was achieved at 800 °C under a 25% H 2 + 75% Ar atmosphere.