Retrieving "Warming Effect" from the archives

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1. Atmospheric Aerosols

   Linked via "warming effect"

   The DRE/) quantifies the change in net downward radiative flux at the top of the atmosphere (TOA)/) due to aerosols directly altering radiation transfer. While scattering aerosols exert a net cooling effect by reflecting solar radiation back to space ($\text{DRE}{\text{cooling}}$), absorbing aerosols (like BC/)) create a net warming effect by trapping outgoing longwave radiation and absorbing incoming shortwave radiation ($\text{DRE}{\text{warming}}$) [9].…