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Radiative forcing is a measure of the influence of a particular factor (e.g.GHGs, aerosols, or land use changes) on the net change in Earth’s energy balance.For example, black carbon aerosols have a positive forcing since they absorb sunlight.Sulfate aerosols have a negative forcing since they reflect sunlight back into space.The country used carbon-free electricity for more than 250 days last year with a continuous 110-day stretch from 17 June until 6 October.
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When the sun’s energy is reflected back into space, Earth avoids warming.
When absorbed energy is released back into space, Earth cools.
On average, a positive radiative forcing tends to warm the surface of the planet, while a negative forcing tends to cool the surface.
GHGs have a positive forcing because they absorb energy radiating from Earth’s surface, rather than allowing it to be directly transmitted into space. Aerosols, or small particles, can have a positive or negative radiative forcing, depending on how they absorb and emit heat or reflect light.