Effects of the aerosols in the temperature retrieval. Top: latitude-pressure cross-sections of the retrieved temperature using the spectral range from 1240 to 1330 cm⁻¹ without including aerosols in the radiative transfer model (Rodríguez-Ovalle et al. 2024). Center: Difference between the temperature profile without hazes and the temperature profile using a 20 mbar haze deck, that is model B* (T_aerosol=0 − T_model–B*). Bottom: difference between the temperature profile without hazes and the temperature profile using a 2 mbar haze deck, that is model A* (T_aerosol=0 − T_model–A*).