Final answer:
The correct answer is a) Longwave; Radiative equilibrium temperature.
Step-by-step explanation:
The correct answer to the question is a) Longwave; Radiative equilibrium temperature.
The relatively constant temperature of the Earth is a result of the energy balance between the incoming solar radiation and the energy radiated from the Earth. Most of the infrared radiation emitted from the Earth is absorbed by CO₂ and H₂O in the atmosphere and then re-radiated back to the Earth or into outer space.
This balance between the absorbed short-wave radiation and the emitted long-wave radiation is known as radiative equilibrium, and the average temperature at which this balance occurs is called the radiative equilibrium temperature.