The interaction of NO(2) with water surfaces in the troposphere is of major interest in atmospheric chemistry. We examined an initial step in this process, the uptake of NO(2) by water through the use of molecular dynamics simulations. An NO(2)-H(2)O intermolecular potential was obtained by fitting to high-level ab initio calculations. We determined the binding of NO(2)-H(2)O to be about two times stronger than that previously calculated. From scattering simulations of an NO(2) molecule interacting with a water slab we observed that the majority of the scattering events resulted in outcomes in which the NO(2) molecule became trapped at the surface or in the interior of the water slab. Typical surface-trapped/adsorbed and bulk-solvated/absorbed trajectories were analyzed to obtain radial distribution functions and the orientational propensity of NO(2) with respect to the water surface. We observed an affinity of the nitrogen atom for the oxygen in water, rather than hydrogen-bonding which was rare. The water solvation shell was less tight for the bulk-absorbed NO(2) than for the surface-adsorbed NO(2). Adsorbed NO(2) demonstrated a marked orientational preference, with the oxygens pointing into the vacuum. Such behavior is expected for a mildly hydrophobic and surfactant molecule like NO(2). Estimates based on our results suggest that at high NO(2) concentrations encountered, for example, in some sampling systems, adsorption and reaction of NO(2) at the surface may contribute to the formation of gas-phase HONO.