CO2 ice is one of the most abundant components in ice-coated interstellar ices besides H2O and CO, but the most favorable path to CO2 ice is still unclear. Molecular dynamics calculations on the ultraviolet photodissociation of different kinds of CO-H2O ice systems have been performed at 10 K in order to demonstrate that the reaction between CO and an OH molecule resulting from H2O photodissociation through the first excited state is a possible route to form CO2 ice. However, our calculations, which take into account different ice surface models, suggest that there is another product with a higher formation probability ((3.00 ± 0.07) × 10(-2)), which is the HOCO complex, whereas the formation of CO2 has a probability of only (3.6 ± 0.7) × 10(-4). The initial location of the CO is key to obtain reaction and form CO2: the CO needs to be located deep into the ice. The HOCO complex becomes trapped in the cold ice surface in the trans-HOCO minimum because it quickly loses its internal energy to the surrounding ice, preventing further reaction to H + CO2. Several laboratory experiments have been carried out recently, and they confirm that CO2 can also be formed through other, different routes. Here we compare our theoretical results with the data available from experiments studying the formation of CO2 through a similar pathway as ours, even though the initial conditions were not exactly the same. Our results also show that the HCO van der Waals complex can be formed through the interaction of CO with the H atom that is formed as a product of H2O photodissociation. Thus, the reaction of the H atom photofragment following H2O photodissociation with CO can be a possible route to form HCO ice.