Increasing the temperature can have a significant impact on the rate of a photochemical reaction involved in the formation of ozone from oxygen molecules. The formation of ozone O3 from oxygen molecules O2 is a three-step process:1. Photodissociation: A high-energy ultraviolet UV photon breaks an oxygen molecule O2 into two oxygen atoms O .O2 + UV photon 2O2. Association: An oxygen atom O reacts with an oxygen molecule O2 to form ozone O3 .O + O2 O33. Dissociation: Ozone absorbs UV radiation and dissociates back into an oxygen molecule and an oxygen atom.O3 + UV photon O2 + OThe overall reaction is:3O2 + UV photon 2O3The rate of a photochemical reaction depends on the number of collisions between reacting molecules and the energy of these collisions. Increasing the temperature increases the kinetic energy of the molecules, which leads to more frequent and energetic collisions. This, in turn, increases the rate of the reaction.However, it is important to note that the formation of ozone is primarily driven by the availability of high-energy UV photons, which are not directly affected by temperature. The rate of photodissociation step 1 depends on the intensity of UV radiation, and this step is usually the rate-limiting step in the formation of ozone.In summary, increasing the temperature can increase the rate of the ozone formation reaction by increasing the kinetic energy of the molecules and the frequency of collisions. However, the overall rate of the reaction is primarily determined by the availability of high-energy UV photons, which are not directly affected by temperature.