Isothermal oxidation of dense TiC ceramics, fabricated by hot‐isostatic pressing at 1630°C and 195 MPa, was performed in Ar/O2 (dry oxidation), Ar/O2/H2O (wet oxidation), and Ar/H2O (H2O oxidation) at 900°–1200°C. The weight change measurements of the TiC specimen showed that the dry, wet, and H2O oxidation at 850°–1000°C is represented by a one‐dimensional parabolic rate equation, while the oxidation in the three atmospheres at 1100° and 1200°C proceeds linearly. Cross‐sectional observation showed that the dry oxidation produces a lamellar TiO2 scale consisting of many thin layers, about 5 μm thick, containing many pores and large cracks, while H2O‐containing oxidation decreases pores in number and diminishes cracks in scales. Gas evolution of CO2 and H2 with weight change measurement was simultaneously followed by heating the TiC to 1400°C in the three atmospheres. Cracking in the TiO2 scale accompanied CO2 evolution, and the H2O‐containing oxidation produced a small amount of H2. A piece of single crystal TiC was oxidized in 16O2/H218O to reveal the contribution of O from H2O to the oxidation of TiC by secondary ion mass spectrometry.