The reaction of gaseous NO with HNO3 on borosilicate glass in the presence of water was studied as a function of surface water coverage at 298 K and a total pressure of one atm in N-2. The loss of gaseous NO and the formation of NO2 were measured in a long path cell using FTIR. The glass walls of the cell provided the surface upon which the chemistry occurred. Water coverages on thin glass cover disks were determined in a separate apparatus by measuring the intensity of the infrared band of liquid water at 3400 cm(-1). Approximately one monolayer was present on the surface at 20% RH and 12 monolayers at 100% RH. The rate of the reaction of NO with HNO3 on the surface was the largest under conditions where approximately three surface monolayers of water were present on the surface. We propose a model for this reaction in which HNO3, added first to the dry cell, hydrogen-bonds to the silanol groups on the surface. The first step in the reaction is believed to be HNO3((surface).) + NO(g) (-->) HONO((surface)) + NO2((g)). Subsequently, HONO on the surface reacts with HNO3 to generate solvated N2O4 as a product. Dissociation of N2O4 generates NO2 as the final gas phase product. This chemistry is potentially important in "renoxification" of the boundary layer of polluted urban atmospheres where silica surfaces are plentiful in particles, soils and building materials, as well as globally in the free troposphere where dust particles are present.