“…Due to the dimension of the perturbers, the first two types of broadening could be considered as two model cases of soft and hard collisional systems, respectively; consequently, they have been employed to test Galatry and Rautian models, whereas O 2 and N 2 broadening are needed to check the evolution of the composition of the atmosphere through a key trace species such as CO, which plays an important role in the global environment. In fact, O 2 and N 2 being the major components of the atmosphere, their pressure broadening coefficients are fundamental for the interpretation of remote sensing data (4,5). In addition, these kinds of experimental data might also be tools for theoreticians in order to test both the accuracy of intermolecular potential energy surfaces and the methodology for connecting the potential energy surface to these observables (see for example Ref.…”