The Global Heat Budget
The Global Heat Budget
basic understanding
- The Global Heat Budget refers to the balance of incoming and outgoing solar radiation that warms the Earth and atmosphere.
- Essentially, it is an expression of how the planet attempts to maintain a delicate energy equilibrium.
- Understanding this, is key to comprehend more complex atmospheric phenomena such as weather patterns, greenhouse effect and climate change.
insolation and albedo
- The Sun's energy, called insolation, reaches Earth's atmosphere and approximately 30% of it is reflected back into space. This is due to albedo, or the reflective properties of different surfaces.
- For example, surfaces such as snow and ice are highly reflective with high albedo rating, while asphalt road or dark forests have lower albedo.
- The remaining 70% of insolation is absorbed by the Earth's surface and atmosphere, warming the planet.
heat transfers: conduction, convection and radiation
- The absorbed solar energy is redistributed around the planet through three methods of heat transfer: conduction, convection, and radiation.
- Conduction is the process of heat transfer from a hot object to a colder one when they come in contact with each other.
- Convection pertains to heat transfer where warm air rises and cool air sinks, making a continuous circulation.
- Radiation is the emission of energy as electromagnetic waves where no physical medium is needed for it to travel.
terrestrial radiation and the greenhouse effect
- As Earth's surface absorbs solar radiation, it also emits radiation back into the atmosphere; this is called terrestrial radiation.
- Some of this re-emitted radiation escapes back into space, but a lot is absorbed by certain gases in atmosphere, known as greenhouse gases, that re-radiate the energy back towards the Earth. This is known as the Greenhouse Effect.
- Some of these greenhouse gases include carbon dioxide (CO2), methane (CH4), and water vapor (H2O).
- This trapping of heat is crucial to supporting life on the planet as it keeps the Earth's average temperature at a habitable level. However, an increase in the concentration of these gases can lead to global warming and climate change.
To summarise, the Global Heat Budget describes the delicate balance of insolation, reflection, absorption, and re-radiation that maintains the Earth's climate. Understanding these points will clarify on how disturbances can lead to significant climatic changes. Be sure to understand the roles of albedo, modes of heat transfer, and the greenhouse effect in this balance.