Energy Balance: Emissivity and Albedo
The Earth’s energy balance is a delicate equilibrium between the energy it receives from the Sun and the energy it radiates back into space.
Two key concepts, emissivity and albedo, play critical roles in this balance.
Emissivity: How Efficiently a Surface Radiates Energy
Emissivity
Emissivity ($e$) measures how efficiently a surface radiates energy compared to an ideal black body.
- A black body is a perfect emitter with an emissivity of 1, meaning it radiates the maximum possible energy at a given temperature.
- Real surfaces have emissivity values between 0 and 1.
- The formula for emissivity is: $$
e = \frac{\text{Power radiated per unit area}}{\sigma T^4}
$$ where:- $e$ is the emissivity.
- $\sigma$ is the Stefan-Boltzmann constant ($5.67 \times 10^{-8} \, \text{W m}^{-2} \text{K}^{-4}$).
- $T$ is the absolute temperature of the surface in Kelvin.

How Emissivity Affects Radiation
- High emissivity: Surfaces with emissivity close to 1, like black bodies, radiate energy efficiently.
- Low emissivity: Surfaces with emissivity near 0, like polished metals, radiate much less energy.
A surface with emissivity $e = 0.8$ radiates 80% of the energy a black body would at the same temperature.
Emissivity in the Real World
Different surfaces have varying emissivity values:
- Oceans: High emissivity (~0.8), radiating energy efficiently.
- Ice: Low emissivity (~0.1), radiating less energy.
Emissivity depends on factors like material composition, surface texture, and temperature.
Albedo: How Much Energy is Reflected
Albedo
Albedo ($\alpha$) measures the reflectivity of a surface.
- It is the fraction of incoming radiation that is reflected back into space.
- The formula for albedo is: $$
\alpha = \frac{\text{Total scattered power}}{\text{Total incident power}}
$$
Albedo values range from 0 (no reflection) to 1 (all radiation is reflected).

How Albedo Affects Energy Balance
- High albedo: Surfaces like snow and ice reflect most of the incoming radiation, contributing to cooler temperatures.
- Low albedo: Surfaces like oceans and forests absorb more radiation, contributing to warmer temperatures.
The Earth’s average albedo is about 0.3, meaning 30% of incoming solar radiation is reflected back into space.
Factors Influencing Albedo
- Surface Type: Snow and ice have high albedo, while forests and oceans have low albedo.
- Cloud Cover: Clouds increase albedo by reflecting sunlight.



