AbstractThe evening transition is crucial in various phenomena, including boundary‐layer stability, temperature inversion, radiation fog, vertical mixing, and pollution dispersion. We have explored this transition using data from 80 days of observations across two fog seasons at the Kempegowda International Airport, Bengaluru (KIAB). Through field experiments and simulations integrating aerosol interaction in a radiation–conduction model, we elucidate the impact of aerosols on longwave cooling of the atmospheric boundary layer (ABL). Field observations indicate that, under calm and clear‐sky conditions, the evening transition typically results in a distinct vertical thermal structure called the lifted temperature minimum (LTM). We observe that the prevailing profile near the surface, post‐sunset is the LTM profile. Additionally, the occurrence of LTM is observed to increase with decreases in downward and upward longwave flux, soil sensible heat flux, wind speed, and turbulent kinetic energy measured at 2 m above ground level (AGL). In such scenarios, the intensity of LTM profiles is governed primarily by the aerosol‐induced longwave heating rate (LHR) within the surface layer. Furthermore, the presence of dense clouds leads to increased downward flux, causing the disappearance of LTM, whereas shallow fog can enhance LTM intensity, as observed in both field observations and simulations. Usually, prevailing radiation models underestimate aerosol‐induced LHR by an order of magnitude compared with actual field observations. We attribute this difference to aerosol‐induced radiation divergence. We show that the impact of aerosol‐induced LHR extends hundreds of meters into the inversion layer, affecting temperature profiles and potentially influencing processes such as fog formation. As the fog layer develops, LHR strengthens at its upper boundary. However, we highlight the difficulty in detecting this cooling using remote instruments such as microwave radiometers.
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