The Earth's energy balance is a crucial concept that describes the balance between incoming energy from the sun and the energy that Earth radiates back into space. This balance determines the planet's climate and overall temperature.
Incoming solar radiation, primarily in the form of visible light, is absorbed by the Earth's surface and atmosphere. This energy is then re-radiated as infrared (heat) energy. To maintain a stable climate, the amount of incoming solar energy must roughly equal the outgoing heat energy.
Disruptions in this balance can lead to climatic changes. For example, if more energy is absorbed than emitted, Earth may experience warming. Factors such as greenhouse gas concentrations and changes in Earth's albedo (reflectivity) can impact this balance.
- The Earth's climate system depends heavily on maintaining this energy balance.
- Human activities, like fossil fuel burning, can upset this balance, contributing to global warming.