We have combined the use of a molecular beam reactor and in situ spectroscopy (XPS) in order to correlate changes in the rate of CO oxidation and the CO–NO reaction with the coverages of the adsorbates and intermediates on the surface. In the reactor, both reactions exhibit an isothermal “light-off” phenomenon in which the rate autocatalytically increases with time. In the case of the CO oxidation reaction this is due to the desorption of CO which releases extra sites for O2 dissociation which, in turn, removes more CO, and hence the acceleration. In effect the reaction can be written as 2COa + O2g + 2S → 2CO2g + 4S, the acceleration coming from the release of extra adsorption sites S, which are involved in the reaction itself. “Fast XPS”, carried out in situ during the course of the reaction, shows domination of the surface by COa below 390 K and domination by Oa above that temperature, with a rapid change in surface coverage over a very narrow temperature window. On high surface area samples this acceleration is further reinforced due to a rapid temperature increase because of the highly exothermic nature of the overall reaction. The situation for the CO–NO reaction is broadly similar, except that the surface is dominated by NO at low temperature, not CO which tends to be displaced from the surface by NO. “Light-off” is dictated by the onset of the dissociation of NOa, which occurs at ∼400 K. Once Na and Oa are formed, N2O production is immediate and accelerates due to the creation of vacant sites for both NO and CO adsorption, the latter removing Oa as CO2g. Again, the reaction self-accelerates and there is a rapid change of surface coverage from NOa to Oa at ∼450 K. The overall self acceleration is due to the following overall reaction, 2NOa + COg + S → N2Og + CO2g + 3S, again producing more adsorption sites (S) in carrying out the reaction step. The rate is reduced at high temperature due to domination of the surface by Oa and to the reduced coverages of the molecular species.