Climate, Surface Energy Flashcards
Net radiation (Q*)
The balance between incoming and outgoing energy at the top of the atmosphere. It is the total energy that is available to influence the climate
Insolation
The solar radiation recieved by a given area
Diurnal cycle
The surface is warmed by a positivie net radiation balance in the daytime, and cooled by a negative radiation balance at night
Heat
Energy transferred along a temperature gradient
What are the three types of heat flux?
1.Sensible
2. Latent
3. Ground heat
Sensible heat flux
Heat that can be felt through the air
Latent heat flux
Heat that is released or absorbed during state changes (condensation and evaporation)
Ground heat flux
Heat that is generated from conduction either within the Earth or on its surface (positive during the day, negative during the night)
What does surface energy budget determine?
Determines how much energy is available to evaporate water and moisten the atmosphere. This energy is redistributed across the globe by the atmosphere and oceans
Equinox
Spring and Autumn Equinoxes which occur when the Earth’s axis is tilted neither towards or away from the Sun, resulting in an equal amount of daylight and darkness across all latitudes
Solstice
Summer Solstice occurs when the Earth’s axis is tilted directly towards the Sun, resulting in longer periods of daylight (vice versa for Winter Solstice)
What are the three impacts of axial tilt on the Earth and Sun’s relationship?
- Daylight hours
- Intensity of solar beam
- Effective atmospheric depth