Kinetic isotope fractionation between water vapor and liquid water or ice depends on the ratio of the diffusivities of the isotopic species in air, but there is disagreement as to the values of these ratios and limited information about their temperature dependence. We use state-of-the-art intermolecular potential-energy surfaces for the water-nitrogen and water-oxygen pairs, along with the kinetic theory of molecular gases, to calculate from first principles the diffusivities of water isotopologues in air. The method has sufficient precision to produce accurate diffusivity ratios. For the HDO/H 2 O ratio, we find that the often used hard-sphere kinetic theory is significantly in error and confirm the 1978 experimental result of Merlivat. For the ratios involving 17 O and 18 O, the simple kinetic theory is relatively close to our more rigorous results. We provide diffusivity ratios from 190 K to 500 K, greatly expanding the range of temperatures for which these ratios are available. Plain Language Summary The different isotopes of hydrogen and oxygen distribute unevenly between water vapor and liquid or solid water during evaporation or precipitation. This fractionation of isotopes is widely used in studies of climate and other geophysical processes. Part of the fractionation depends on the relative diffusion rates of the isotopic molecules in air, but these relative diffusivities are difficult to measure and existing data are inconsistent. Because of these inconsistencies, a simple theory that treats the molecules as hard spheres is often used. We used more rigorous theory based on detailed quantum-mechanical description of the interactions between water molecules and those of nitrogen and oxygen to calculate the diffusivity ratios. Our results confirm some previous experiments and show that the simple hard-sphere model is not accurate. They also provide diffusivity ratios at temperatures where no experimental data exist, such as those relevant to ice.