Atmospheric aerosols play a crucial role in modulating the energy available to the Earth’s surface, influencing the hydrological cycle, ecosystems, and climate. In the Amazon, previous studies have mainly examined how aerosols scatter and absorb radiation, enhancing diffuse radiation and influencing gross primary productivity. However, little is known about their interactions with energy partitioning (i.e., sensible and latent heat fluxes). Here, we investigate how regimes of high (AOD > 0.40) and low (AOD < 0.13) aerosol optical depth (AOD) affect surface energy and carbon dioxide (CO₂) fluxes in an undisturbed Amazon rainforest. For this, we used long-term meteorological measurements from the Amazon Tall Tower Observatory (ATTO) collected between 2016 and 2022. We find that enhanced aerosol presence reduces both sensible heat flux and energy available for evapotranspiration by approximately 10 %, while decreasing CO₂ fluxes by about 58 %, which suggests enhanced carbon assimilation by the forest. The impact of aerosols on turbulent surface fluxes is reflected in a cooling of approximately 0.5 °C at the canopy top, caused by a 5.6 % reduction in incoming shortwave radiation. These results demonstrate that aerosols modify turbulent energy exchange, with consequences for the forest microclimate and the coupled carbon and water cycles. It highlights the critical role of aerosols in the functioning of the ecosystem.